首页 > 最新文献

Soil & Tillage Research最新文献

英文 中文
Plastic film mulching with nitrogen application activates rhizosphere microbial nitrification and dissimilatory nitrate reduction in the Loess Plateau 地膜覆氮激活黄土高原根际微生物硝化作用和异化态硝酸盐还原
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-25 DOI: 10.1016/j.still.2024.106423
Congwei Sun , Hui Wu , Subramaniam Gopalakrishnan , Enke Liu , Xurong Mei
Plastic film mulching combined with nitrogen application is a prime chief strategy for enhancing maize yields in rain-fed agricultural areas. However, how the practice affects the productivity and functions of soil by altering nitrogen transformation mediated by rhizosphere microorganisms in the Loess Plateau, remains unclear. In this research, an 7-year field location experiment was conducted to ascertain the effects of plastic film mulching with nitrogen application (225 kg N ha−1) on the rhizosphere microbial nitrogen transformation in a rain-fed maize field on the Loess Plateau. Plastic film mulching with nitrogen application reduced the pH value and also increased the abundance of microorganisms (e.g., Nitrosospira, Halomonas) and genes (e.g., pmoB-amoB, hao, nirB, and nirD) during the vegetative stage. This promoted nitrification and dissimilatory nitrate reduction to ammonium, which increased the content of inorganic nitrogen in the rhizosphere. During the reproductive stages, plastic flim mulching reduced the relative abundance of aerobic bacteria (e.g., Skermanella, Sphingomonas), and the ratio of (nirK + nirS) / nosZ, which inhibited denitrification and dinitrogen oxide emission potential. Overall, our findings highlight the feedback mechanism of soil nitrogen transformation to plastic film mulching with nitrogen application in the Loess Plateau, providing valuable insights for manipulating specific microorganisms to regulate nitrogen transformation and promoting the sustainability of soil ecosystems.
在雨养农业区,覆膜配施氮肥是提高玉米产量的主要策略。然而,这种做法如何通过改变黄土高原根际微生物介导的氮转化来影响土壤的生产力和功能尚不清楚。本研究通过为期7年的田间定位试验,研究了覆膜施氮(225 kg N ha−1)对黄土高原旱作玉米根际微生物氮转化的影响。覆盖地膜施氮降低了土壤的pH值,也增加了营养阶段微生物(如亚硝基螺旋体、盐单胞菌)和基因(如pmoB-amoB、hao、nirB和nirD)的丰度。这促进了硝化作用和异化硝态氮还原为铵态氮,从而增加了根际无机氮的含量。在繁殖阶段,地膜覆盖降低了好氧菌(Skermanella,鞘氨单胞菌)的相对丰度和(nirK + nirS) / nosZ的比值,从而抑制了反硝化作用和二氮氧化物排放势。综上所述,本研究揭示了黄土高原土壤氮素向地膜转化的反馈机制,为调控特定微生物调控氮素转化,促进土壤生态系统的可持续性提供了有价值的见解。
{"title":"Plastic film mulching with nitrogen application activates rhizosphere microbial nitrification and dissimilatory nitrate reduction in the Loess Plateau","authors":"Congwei Sun ,&nbsp;Hui Wu ,&nbsp;Subramaniam Gopalakrishnan ,&nbsp;Enke Liu ,&nbsp;Xurong Mei","doi":"10.1016/j.still.2024.106423","DOIUrl":"10.1016/j.still.2024.106423","url":null,"abstract":"<div><div>Plastic film mulching combined with nitrogen application is a prime chief strategy for enhancing maize yields in rain-fed agricultural areas. However, how the practice affects the productivity and functions of soil by altering nitrogen transformation mediated by rhizosphere microorganisms in the Loess Plateau, remains unclear. In this research, an 7-year field location experiment was conducted to ascertain the effects of plastic film mulching with nitrogen application (225 kg N ha<sup>−1</sup>) on the rhizosphere microbial nitrogen transformation in a rain-fed maize field on the Loess Plateau. Plastic film mulching with nitrogen application reduced the pH value and also increased the abundance of microorganisms (e.g., <em>Nitrosospira</em>, <em>Halomonas</em>) and genes (e.g., <em>pmoB-amoB</em>, <em>hao</em>, <em>nirB</em>, and <em>nirD</em>) during the vegetative stage. This promoted nitrification and dissimilatory nitrate reduction to ammonium, which increased the content of inorganic nitrogen in the rhizosphere. During the reproductive stages, plastic flim mulching reduced the relative abundance of aerobic bacteria (e.g., <em>Skermanella</em>, <em>Sphingomonas</em>), and the ratio of (<em>nirK</em> + <em>nirS</em>) / <em>nosZ</em>, which inhibited denitrification and dinitrogen oxide emission potential. Overall, our findings highlight the feedback mechanism of soil nitrogen transformation to plastic film mulching with nitrogen application in the Loess Plateau, providing valuable insights for manipulating specific microorganisms to regulate nitrogen transformation and promoting the sustainability of soil ecosystems.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106423"},"PeriodicalIF":6.1,"publicationDate":"2024-12-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889229","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Non-leguminous green manures improve labile phosphorus availability and crop yield in agroecosystems: A global meta-analysis 非豆科绿肥提高农业生态系统中不稳定磷的有效性和作物产量:一项全球荟萃分析
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-24 DOI: 10.1016/j.still.2024.106430
Adnan Anwar Khan , Imran Azeem , Jing Hui , Yupei Chen , Yuqi Yuan , Tahir Shah , Muhammad Adeel , Noman Shakoor , Rana Muhammad Ammar Asghar , Weidong Cao , Dabin Zhang , Yajun Gao
Incorporating the green manure (GM) approach in agroecosystems enhances phosphorus (P) availability and reduces mineral P-fertilizer input. Despite global promotion, a comprehensive global synthesis of the GM effect on soil P fractions is lacking. To address this gap, we conducted a meta-analysis of 48 published studies to evaluate the impact of climatic, edaphic, and agronomic variables on soil P fractions, enzyme activities, subsequent crop yield, and P uptake under a GM cropping system. Overall, GMs significantly increased the labile P fraction (n = 592) by 18 % compared with fallow management. Non-leguminous GMs showed a 21 % increase in labile P, resulting in an 18 % increase in subsequent crop yield and a 30 % increase in subsequent crop P uptake compared with fallow. Leguminous GMs stimulated soil enzyme activities, elevating acid phosphatase (ACP) by 40 % and β-glucosidase by 182 % compared with fallow. Compared to no-till (NT), GMs under conventional tillage (CT) significantly increased soil enzyme activities, including ACP, alkaline phosphatase (ALP), β-glucosidase, as well as subsequent crop yield, and P uptake. Long-term GM incorporation (5–10 yrs) significantly reduced moderately labile P by 25 %, leading to increased labile P fraction. Linear regression analysis demonstrated a positive correlation between labile P and soil organic carbon (SOC), but a negative with mean annual precipitation (MAP) and mean annual temperature (MAT). These findings suggest that incorporating GMs into a CT management system can potentially accelerate soil P cycling by promoting soil enzyme activities, enhancing subsequent crop production, and providing an alternative approach to reducing mineral P-fertilizer dependency. This approach exemplifies sustainable food production practices and underscores the significance of GMs for long-term agricultural resilience and soil health worldwide.
在农业生态系统中引入绿肥(GM)方法可以提高磷(P)的有效性,并减少矿物磷肥的投入。尽管在全球推广,但缺乏对转基因对土壤磷组分影响的全面全球综合。为了解决这一差距,我们对48项已发表的研究进行了荟萃分析,以评估气候、土壤和农艺变量对转基因种植系统下土壤磷组分、酶活性、后续作物产量和磷吸收的影响。总体而言,与休耕管理相比,转基因显著提高了不稳定P分数(n = 592)18 %。与休耕相比,非豆科转基因作物增加了21 %的活性磷,导致后续作物产量增加18 %,后续作物磷吸收量增加30 %。豆科转基因作物刺激土壤酶活性,与休耕相比,酸性磷酸酶(ACP)和β-葡萄糖苷酶分别提高了40% %和182 %。与免耕(NT)相比,常规耕作(CT)下转基因作物显著提高了土壤ACP、碱性磷酸酶(ALP)、β-葡萄糖苷酶(β-葡萄糖苷酶)活性,以及随后的作物产量和磷素吸收。长期加入转基因(5-10 年)显著降低了25 %的中度不稳定磷,导致不稳定磷比例增加。线性回归分析表明,土壤活性磷与土壤有机碳(SOC)呈正相关,与年平均降水量(MAP)和年平均气温(MAT)呈负相关。这些发现表明,将转基因作物纳入CT管理系统可以通过促进土壤酶活性,提高后续作物产量,并提供一种减少矿物磷肥依赖的替代方法,从而潜在地加速土壤磷循环。这种方法体现了可持续粮食生产实践,并强调了转基因作物对全球农业长期恢复力和土壤健康的重要性。
{"title":"Non-leguminous green manures improve labile phosphorus availability and crop yield in agroecosystems: A global meta-analysis","authors":"Adnan Anwar Khan ,&nbsp;Imran Azeem ,&nbsp;Jing Hui ,&nbsp;Yupei Chen ,&nbsp;Yuqi Yuan ,&nbsp;Tahir Shah ,&nbsp;Muhammad Adeel ,&nbsp;Noman Shakoor ,&nbsp;Rana Muhammad Ammar Asghar ,&nbsp;Weidong Cao ,&nbsp;Dabin Zhang ,&nbsp;Yajun Gao","doi":"10.1016/j.still.2024.106430","DOIUrl":"10.1016/j.still.2024.106430","url":null,"abstract":"<div><div>Incorporating the green manure (GM) approach in agroecosystems enhances phosphorus (P) availability and reduces mineral P-fertilizer input. Despite global promotion, a comprehensive global synthesis of the GM effect on soil P fractions is lacking. To address this gap, we conducted a meta-analysis of 48 published studies to evaluate the impact of climatic, edaphic, and agronomic variables on soil P fractions, enzyme activities, subsequent crop yield, and P uptake under a GM cropping system. Overall, GMs significantly increased the labile P fraction (n = 592) by 18 % compared with fallow management. Non-leguminous GMs showed a 21 % increase in labile P, resulting in an 18 % increase in subsequent crop yield and a 30 % increase in subsequent crop P uptake compared with fallow. Leguminous GMs stimulated soil enzyme activities, elevating acid phosphatase (ACP) by 40 % and β-glucosidase by 182 % compared with fallow. Compared to no-till (NT), GMs under conventional tillage (CT) significantly increased soil enzyme activities, including ACP, alkaline phosphatase (ALP), β-glucosidase, as well as subsequent crop yield, and P uptake. Long-term GM incorporation (5–10 yrs) significantly reduced moderately labile P by 25 %, leading to increased labile P fraction. Linear regression analysis demonstrated a positive correlation between labile P and soil organic carbon (SOC), but a negative with mean annual precipitation (MAP) and mean annual temperature (MAT). These findings suggest that incorporating GMs into a CT management system can potentially accelerate soil P cycling by promoting soil enzyme activities, enhancing subsequent crop production, and providing an alternative approach to reducing mineral P-fertilizer dependency. This approach exemplifies sustainable food production practices and underscores the significance of GMs for long-term agricultural resilience and soil health worldwide.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106430"},"PeriodicalIF":6.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889232","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Space-time mapping of soil organic carbon through remote sensing and machine learning 基于遥感和机器学习的土壤有机碳时空制图
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-24 DOI: 10.1016/j.still.2024.106428
Bruno dos Anjos Bartsch , Nicolas Augusto Rosin , Jorge Tadeu Fim Rosas , Raul Roberto Poppiel , Fernando Yutaro Makino , Letícia Guadagnin Vogel , Jean Jesus Macedo Novais , Renan Falcioni , Marcelo Rodrigo Alves , José A.M. Demattê
Pedosphere is the largest terrestrial carbon reservoir. Soil organic carbon (SOC) is a critical attribute for soil quality and crop productivity, being directly linked to climate change mitigation and food security. Brazil boasts a significant agricultural production area and substantial potential for carbon sequestration. Nevertheless, the spatial-temporal distribution of SOC across the country is poorly understood, hindering the implementation of low-carbon agriculture public policies. We aimed to map the spatio-temporal distribution of SOC at from 0.00 to 0.20 cm depth over two periods. We assessed the SOC variation over seven years, generating a time series with five periods, obtaining the average SOC values. The Cubist algorithm was used to calibrate two short period (two years) and a long period (seven years/all period) models for SOC spatial prediction. Remote sensing data and soil particle size distribution maps were used as environmental covariates. We found in validation R2 values of 0.47 and 0.25 for short period models, and 0.34 for the long period model. The SOC content decreased by 54.97 % in the area according to the mapping by short period models and 53.72 % according to mapping by the long-period model. The predicted maps showed the same trend of the database (soil samples with observed SOC values) for the study areas using both short period and long period models.
土壤圈是最大的陆地碳库。土壤有机碳(SOC)是土壤质量和作物生产力的关键属性,与减缓气候变化和粮食安全直接相关。巴西拥有巨大的农业生产面积和巨大的碳封存潜力。然而,目前对全国有机碳的时空分布知之甚少,阻碍了低碳农业公共政策的实施。我们的目的是绘制在0.00 ~ 0.20 cm深度两个时间段内土壤有机碳的时空分布。我们评估了7年的SOC变化,生成了5个周期的时间序列,得到了平均SOC值。利用Cubist算法分别对两种短期(2年)和长期(7年/全期)土壤有机碳空间预测模型进行了标定。采用遥感数据和土壤粒度分布图作为环境协变量。我们在验证中发现,短期模型的R2值为0.47和0.25,长期模型的R2值为0.34。根据短周期模型和长周期模型,该地区有机碳含量分别下降了54.97 %和53.72 %。在短周期模型和长周期模型的预测图中,研究区土壤有机碳的变化趋势相同。
{"title":"Space-time mapping of soil organic carbon through remote sensing and machine learning","authors":"Bruno dos Anjos Bartsch ,&nbsp;Nicolas Augusto Rosin ,&nbsp;Jorge Tadeu Fim Rosas ,&nbsp;Raul Roberto Poppiel ,&nbsp;Fernando Yutaro Makino ,&nbsp;Letícia Guadagnin Vogel ,&nbsp;Jean Jesus Macedo Novais ,&nbsp;Renan Falcioni ,&nbsp;Marcelo Rodrigo Alves ,&nbsp;José A.M. Demattê","doi":"10.1016/j.still.2024.106428","DOIUrl":"10.1016/j.still.2024.106428","url":null,"abstract":"<div><div>Pedosphere is the largest terrestrial carbon reservoir. Soil organic carbon (SOC) is a critical attribute for soil quality and crop productivity, being directly linked to climate change mitigation and food security. Brazil boasts a significant agricultural production area and substantial potential for carbon sequestration. Nevertheless, the spatial-temporal distribution of SOC across the country is poorly understood, hindering the implementation of low-carbon agriculture public policies. We aimed to map the spatio-temporal distribution of SOC at from 0.00 to 0.20 cm depth over two periods. We assessed the SOC variation over seven years, generating a time series with five periods, obtaining the average SOC values. The Cubist algorithm was used to calibrate two short period (two years) and a long period (seven years/all period) models for SOC spatial prediction. Remote sensing data and soil particle size distribution maps were used as environmental covariates. We found in validation R<sup>2</sup> values of 0.47 and 0.25 for short period models, and 0.34 for the long period model. The SOC content decreased by 54.97 % in the area according to the mapping by short period models and 53.72 % according to mapping by the long-period model. The predicted maps showed the same trend of the database (soil samples with observed SOC values) for the study areas using both short period and long period models.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106428"},"PeriodicalIF":6.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889104","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
How do different ant species mediate CH4 fluxes in slash-burn tropical forest soils? 不同蚁种如何调节刀耕火种热带森林土壤中CH4的通量?
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-24 DOI: 10.1016/j.still.2024.106432
Lingling Xie , Shaojun Wang , Mei Lu , Bo Xiao , Zhengjun Wang , Zhipeng Guo , Xiaofei Guo , Shuang Luo , Ru Li , Jiahui Xia , Shengqiu Yang , Mengjie Lan
As important structuring force in ecosystems, ants play crucial roles in driving source-sink processes of soil methane (CH4) through a series of biotic and abiotic pathways. However, there is still uncertainty about how different ant species regulate CH4 fluxes in slash-burn tropical soils. This study aimed to identify the pathways by which the different ant species (i.e., Pheidole capellini-honeydew harvester, Odontoponera transversa-predator, and Pheidologeton affinis-scavenger) control soil CH4 fluxes in Xishuangbanna tropical forests, southwestern China. We observed a net CH4 emission in the nests of three ant species (1.29 ± 0.047 μg m−2 h−1) and a net uptake in the reference soils (-1.60 ± 0.043 μg m−2 h−1). The contribution of three ant species to the reduction of annual total forest surface CH4 uptake ranged from 0.06 % to 4.82 %. The P. capellini nests increased CH4 emissions by 144.18 % compared with the reference soils, whereas O. transversa and P. affinis nests increased by 124.65 % and 111.71 %, respectively. In contrast with the reference soils, the greatest increase (33.7–511.1 %) in abundance of dominant methanogen taxa (Candidatus Thermoplasmatota and Euryarchaeota), methanogen Sobs index, soil water content, total organic carbon, and microbial biomass carbon was found in P. capellini nests. In contrast, the highest increase (92.0 %) in nitrate nitrogen was recorded in P. affinis nests. In particular, CH4 fluxes were directly or indirectly driven by increased Candidatus Thermoplasmatota abundance (26.04 %), soil water content (15.41 %), and microbial biomass carbon (11.70 %), while the abundance of Methylomirabilota bacteria explained 7.76 % of variation in CH4 fluxes. Our data indicate that CH4 fluxes vary with ant species probably due to their differentiated modification on methanogenic bacterial abundance, micro-habitat, and microbial carbon in Xishuangbann tropical soils. This results would provide further insight into the contribution of soil fauna to greenhouse gas emissions from tropical forests.
蚂蚁作为生态系统中重要的结构力量,通过一系列生物和非生物途径,在驱动土壤甲烷(CH4)源库过程中起着至关重要的作用。然而,关于不同蚂蚁物种如何调节刀耕火种热带土壤中的CH4通量仍然存在不确定性。本研究旨在探讨西双版纳热带森林不同蚁种(Pheidole capellini-honeydew harvester, Odontoponera -横掠捕食者和Pheidologeton affin食腐者)控制土壤CH4通量的途径。我们观察到三种蚂蚁巢穴的CH4净排放量(1.29 ± 0.047 μg m−2 h−1)和参考土壤的净吸收率(-1.60 ± 0.043 μg m−2 h−1)。3种蚂蚁对减少森林年地表CH4总吸收率的贡献范围为0.06 % ~ 4.82 %。与对照土壤相比,capellini土壤的CH4排放量增加了144.18 %,而o.s transversa和affinis土壤的CH4排放量分别增加了124.65 %和111.71 %。与对照土壤相比,P. capellini巢穴的优势产甲烷菌群(Candidatus Thermoplasmatota和Euryarchaeota)丰度、产甲烷菌Sobs指数、土壤含水量、总有机碳和微生物生物量碳增加幅度最大(33.7-511.1 %)。与此相反,亲和燕窝中硝酸盐氮的增幅最高(92.0 %)。特别是,CH4通量直接或间接受到热浆候选菌丰度(26.04 %)、土壤含水量(15.41 %)和微生物生物量碳(11.70 %)增加的驱动,而甲基化菌丰度解释了CH4通量变化的7.76 %。研究结果表明,不同蚁种对西双版市热带土壤甲烷细菌丰度、微生境和微生物碳的不同影响可能导致了CH4通量的变化。这一结果将进一步深入了解土壤动物对热带森林温室气体排放的贡献。
{"title":"How do different ant species mediate CH4 fluxes in slash-burn tropical forest soils?","authors":"Lingling Xie ,&nbsp;Shaojun Wang ,&nbsp;Mei Lu ,&nbsp;Bo Xiao ,&nbsp;Zhengjun Wang ,&nbsp;Zhipeng Guo ,&nbsp;Xiaofei Guo ,&nbsp;Shuang Luo ,&nbsp;Ru Li ,&nbsp;Jiahui Xia ,&nbsp;Shengqiu Yang ,&nbsp;Mengjie Lan","doi":"10.1016/j.still.2024.106432","DOIUrl":"10.1016/j.still.2024.106432","url":null,"abstract":"<div><div>As important structuring force in ecosystems, ants play crucial roles in driving source-sink processes of soil methane (CH<sub>4</sub>) through a series of biotic and abiotic pathways. However, there is still uncertainty about how different ant species regulate CH<sub>4</sub> fluxes in slash-burn tropical soils. This study aimed to identify the pathways by which the different ant species (i.e., <em>Pheidole capellini</em>-honeydew harvester, <em>Odontoponera transversa</em>-predator, and <em>Pheidologeton affinis</em>-scavenger) control soil CH<sub>4</sub> fluxes in Xishuangbanna tropical forests, southwestern China. We observed a net CH<sub>4</sub> emission in the nests of three ant species (1.29 ± 0.047 μg m<sup>−2</sup> h<sup>−1</sup>) and a net uptake in the reference soils (-1.60 ± 0.043 μg m<sup>−2</sup> h<sup>−1</sup>). The contribution of three ant species to the reduction of annual total forest surface CH<sub>4</sub> uptake ranged from 0.06 % to 4.82 %. The <em>P. capellini</em> nests increased CH<sub>4</sub> emissions by 144.18 % compared with the reference soils, whereas <em>O. transversa</em> and <em>P. affinis</em> nests increased by 124.65 % and 111.71 %, respectively. In contrast with the reference soils, the greatest increase (33.7–511.1 %) in abundance of dominant methanogen taxa (Candidatus Thermoplasmatota and Euryarchaeota), methanogen Sobs index, soil water content, total organic carbon, and microbial biomass carbon was found in <em>P. capellini</em> nests. In contrast, the highest increase (92.0 %) in nitrate nitrogen was recorded in <em>P. affinis</em> nests. In particular, CH<sub>4</sub> fluxes were directly or indirectly driven by increased Candidatus Thermoplasmatota abundance (26.04 %), soil water content (15.41 %), and microbial biomass carbon (11.70 %), while the abundance of Methylomirabilota bacteria explained 7.76 % of variation in CH<sub>4</sub> fluxes. Our data indicate that CH<sub>4</sub> fluxes vary with ant species probably due to their differentiated modification on methanogenic bacterial abundance, micro-habitat, and microbial carbon in Xishuangbann tropical soils. This results would provide further insight into the contribution of soil fauna to greenhouse gas emissions from tropical forests.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106432"},"PeriodicalIF":6.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889105","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Synergistic effects of bio-organic fertilizer and different soil amendments on salt reduction, soil fertility, and yield enhancement in salt-affected coastal soils 生物有机肥与不同土壤改良剂对滨海盐渍化土壤减盐、肥力和增产的协同效应
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-24 DOI: 10.1016/j.still.2024.106433
Meng Xiao , Shengguo Jiang , Jinbiao Li , Wenping Li , Pengxiao Fu , Guangming Liu , Jinlin Chen
Soil salinization is associated with soil productivity and food stocks, and hazards to the sustainable development of agriculture economics and the ecological environment. Hence, to evaluate the improvement and underlying mechanisms of agricultural amelioration practices on salinity alleviation, soil fertility improvement and crop growth, the organic fertilizer and soil amendments were applied to the rice field in coastal saline soil over one year. In this study, five treatments replicated three times were conducted in 15 experimental plots including CK (no amendments addition), OF (bio-organic fertilizer addition), OH (bio-organic fertilizer combined with hydrolytic polymaleic anhydride addition), OQ (bio-organic fertilizer combined with carbon nano sol addition), OB (bio-organic fertilizer combined with potassium fulvic acid addition). Co-application of organic fertilizer and soil amendment significantly reduced soil pH and EC by 1.3 % - 3.7 % and 14 % - 20 %, respectively. Organic treatments OH has the highest content of SOC (10.46 g kg−1) and available nitrogen (AN, 76 mg kg−1). OB treatment has the highest content of available potassium (AK, 294 mg kg−1), and the activity of soil urease (S-UE) and alkaline phosphatase (S-AKP). Organic treatments have significantly increased the plant height, leaf area, 1000-grain weight (4 %-7 %), and yield of rice (4 %-15 %) compared to CK. Organic fertilizer and amendments added explained 81 % and 68 % of the variation in SQI and rice yield, respectively. RDA analysis indicated that S-UE activity and nitrogen were the most factors that contributed to SQI and rice yield. Our results suggested that the organic fertilizer combined with soil amendments improved soil quality comprehensively, and enhanced rice growth and yield by reducing soil salt and salinity, and increasing soil biochemical properties (S-UE and N content) in coastal saline soil.
土壤盐渍化关系到土壤生产力和粮食储量,对农业经济和生态环境的可持续发展造成危害。因此,为了评价农业改良措施对减轻盐碱化、提高土壤肥力和作物生长的改善作用及其潜在机制,在沿海盐碱地稻田施用了一年多的有机肥和土壤改良剂。本研究在15个试验区进行了CK(不添加改良剂)、OF(生物有机肥添加)、OH(生物有机肥与水解聚丁二烯酸酐添加)、OQ(生物有机肥与碳纳米溶胶添加)、OB(生物有机肥与富里酸钾添加)5个重复3次的处理。施用有机肥和土壤改良剂可显著降低土壤pH和EC,分别降低1.3 % ~ 3.7 %和14 % ~ 20 %。有机处理OH的有机有机碳含量最高(10.46 g kg−1),速效氮含量最高(76 mg kg−1)。OB处理土壤速效钾含量最高(294 mg kg−1),土壤脲酶(S-UE)和碱性磷酸酶(S-AKP)活性最高。与对照相比,有机处理显著提高了水稻株高、叶面积、千粒重(4 % ~ 7 %)和产量(4 % ~ 15 %)。添加有机肥和改良剂对SQI和水稻产量的贡献率分别为81% %和68% %。RDA分析表明,S-UE活性和氮素是影响SQI和水稻产量的主要因子。结果表明,有机肥配施土壤改良剂能全面改善土壤质量,通过降低土壤盐分和矿化度,提高土壤生化特性(S-UE和N含量),促进沿海盐碱地水稻生长和产量。
{"title":"Synergistic effects of bio-organic fertilizer and different soil amendments on salt reduction, soil fertility, and yield enhancement in salt-affected coastal soils","authors":"Meng Xiao ,&nbsp;Shengguo Jiang ,&nbsp;Jinbiao Li ,&nbsp;Wenping Li ,&nbsp;Pengxiao Fu ,&nbsp;Guangming Liu ,&nbsp;Jinlin Chen","doi":"10.1016/j.still.2024.106433","DOIUrl":"10.1016/j.still.2024.106433","url":null,"abstract":"<div><div>Soil salinization is associated with soil productivity and food stocks, and hazards to the sustainable development of agriculture economics and the ecological environment. Hence, to evaluate the improvement and underlying mechanisms of agricultural amelioration practices on salinity alleviation, soil fertility improvement and crop growth, the organic fertilizer and soil amendments were applied to the rice field in coastal saline soil over one year. In this study, five treatments replicated three times were conducted in 15 experimental plots including CK (no amendments addition), OF (bio-organic fertilizer addition), OH (bio-organic fertilizer combined with hydrolytic polymaleic anhydride addition), OQ (bio-organic fertilizer combined with carbon nano sol addition), OB (bio-organic fertilizer combined with potassium fulvic acid addition). Co-application of organic fertilizer and soil amendment significantly reduced soil pH and EC by 1.3 % - 3.7 % and 14 % - 20 %, respectively. Organic treatments OH has the highest content of SOC (10.46 g kg<sup>−1</sup>) and available nitrogen (AN, 76 mg kg<sup>−1</sup>). OB treatment has the highest content of available potassium (AK, 294 mg kg<sup>−1</sup>), and the activity of soil urease (S-UE) and alkaline phosphatase (S-AKP). Organic treatments have significantly increased the plant height, leaf area, 1000-grain weight (4 %-7 %), and yield of rice (4 %-15 %) compared to CK. Organic fertilizer and amendments added explained 81 % and 68 % of the variation in SQI and rice yield, respectively. RDA analysis indicated that S-UE activity and nitrogen were the most factors that contributed to SQI and rice yield. Our results suggested that the organic fertilizer combined with soil amendments improved soil quality comprehensively, and enhanced rice growth and yield by reducing soil salt and salinity, and increasing soil biochemical properties (S-UE and N content) in coastal saline soil.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106433"},"PeriodicalIF":6.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889231","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Impacts of landscape factors on gully retreat and its morphological characteristics in hilly areas of Northeast China 景观因子对东北丘陵区沟壑退缩的影响及其形态特征
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-24 DOI: 10.1016/j.still.2024.106434
Peng Jiao , Yang Ou , Shujiang Pang , Baixing Yan , Yu Zhang , Wenxu Xu , Liming Yan
The black soil region in Northeast China is an important commodity grain base. In recent years, with the intensification of agricultural activities, the formation and development of gullies on sloping farmland have accelerated, severely affecting food and ecological security. In order to effectively control regional soil erosion, this study comprehensively utilized historical databases of gullies, remote sensing images, field surveys, spatial analysis, and multivariate statistical techniques to reveal the morphological characteristics, development rates, and main driving factors of 116 gullies in typical agricultural watersheds in the low hills of Northeast China. The results showed that linear gully retreat rate in the study area ranged from 4.3 to 8.4 m y−1, with an average of approximately 6.34 m y−1, between 2011 and 2021. The areal gully retreat rate ranged from 90.7 to 1224.4 m2 y−1, with an average growth rate of approximately 339.17 m2 y−1. Compared with other regions in the world, the development rate of gullies in black soil region of Northeast China is relatively fast, especially in terms of lateral expansion, which is about 7 times greater than longitudinal extension. Gully side-wall retreat (approximately 56.8 m2 y−1) was found to be the dominant factor influencing the change in gully area. Environmental variables explained 60.2 % of the variation in gully morphological characteristics, with natural factors having a greater impact on the linear development of gullies than human factors. However, human factors were closely related to lateral expansion. Due to the large proportion of agricultural landscapes and high spatial homogeneity in the study area, micro-topographic features (such as catchment area and elevation) and the spatial configuration of agricultural landscape patches (patch density and edge density) were identified as the main influencing factors of gully erosion development in study area. Therefore, targeted measures and control strategies should be designed based on a comprehensive assessment of terrain factors and landscape pattern indicators to mitigate gully erosion risks. In the future, based on obtaining more three-dimensional data of gullies, empirical coefficient equations should be constructed using gully area and length as independent variables to predict gully volume. This will help identify the main factors influencing sediment and organic matter loss caused by gully erosion in black soil region, and provide technical support for improving the predictive capabilities of gully erosion risks and developing more rational prevention and control strategies.
东北黑土地区是中国重要的商品粮基地。近年来,随着农业活动的加剧,坡耕地沟壑的形成和发展加快,严重影响了粮食安全与生态安全。为了有效控制区域土壤侵蚀,综合利用沟壑历史数据库、遥感影像、野外调查、空间分析和多元统计等技术,揭示了东北低丘典型农业流域116条沟壑的形态特征、发育速率及其主要驱动因素。结果表明:2011 - 2021年,研究区沟谷退缩率为4.3 ~ 8.4 m y−1,平均约为6.34 m y−1;沟面退缩率为90.7 ~ 1224.4 m2 y−1,平均生长率约为339.17 m2 y−1。与世界其他地区相比,东北黑土区沟槽发育速度较快,特别是横向扩展速度约为纵向扩展速度的7倍。沟槽侧壁退缩(约56.8 m2 y−1)是影响沟槽面积变化的主要因素。环境变量对沟壑形态特征变化的贡献率为60.2 %,自然因素对沟壑线性发育的影响大于人为因素。然而,人为因素与侧方扩张密切相关。研究区农业景观占比大,空间均匀性高,微地形特征(流域面积、高程)和农业景观斑块的空间配置(斑块密度、边缘密度)是影响研究区沟蚀发展的主要因素。因此,应在综合评价地形因素和景观格局指标的基础上,设计有针对性的措施和控制策略,以减轻沟壑区侵蚀风险。今后,在获取更多沟槽三维数据的基础上,应以沟槽面积和沟槽长度为自变量,构建经验系数方程来预测沟槽体积。这将有助于识别黑土区沟蚀导致泥沙和有机质流失的主要影响因素,为提高沟蚀风险预测能力和制定更合理的防治策略提供技术支持。
{"title":"Impacts of landscape factors on gully retreat and its morphological characteristics in hilly areas of Northeast China","authors":"Peng Jiao ,&nbsp;Yang Ou ,&nbsp;Shujiang Pang ,&nbsp;Baixing Yan ,&nbsp;Yu Zhang ,&nbsp;Wenxu Xu ,&nbsp;Liming Yan","doi":"10.1016/j.still.2024.106434","DOIUrl":"10.1016/j.still.2024.106434","url":null,"abstract":"<div><div>The black soil region in Northeast China is an important commodity grain base. In recent years, with the intensification of agricultural activities, the formation and development of gullies on sloping farmland have accelerated, severely affecting food and ecological security. In order to effectively control regional soil erosion, this study comprehensively utilized historical databases of gullies, remote sensing images, field surveys, spatial analysis, and multivariate statistical techniques to reveal the morphological characteristics, development rates, and main driving factors of 116 gullies in typical agricultural watersheds in the low hills of Northeast China. The results showed that linear gully retreat rate in the study area ranged from 4.3 to 8.4 m y<sup>−1</sup>, with an average of approximately 6.34 m y<sup>−1</sup>, between 2011 and 2021. The areal gully retreat rate ranged from 90.7 to 1224.4 m<sup>2</sup> y<sup>−1</sup>, with an average growth rate of approximately 339.17 m<sup>2</sup> y<sup>−1</sup>. Compared with other regions in the world, the development rate of gullies in black soil region of Northeast China is relatively fast, especially in terms of lateral expansion, which is about 7 times greater than longitudinal extension. Gully side-wall retreat (approximately 56.8 m<sup>2</sup> y<sup>−1</sup>) was found to be the dominant factor influencing the change in gully area. Environmental variables explained 60.2 % of the variation in gully morphological characteristics, with natural factors having a greater impact on the linear development of gullies than human factors. However, human factors were closely related to lateral expansion. Due to the large proportion of agricultural landscapes and high spatial homogeneity in the study area, micro-topographic features (such as catchment area and elevation) and the spatial configuration of agricultural landscape patches (patch density and edge density) were identified as the main influencing factors of gully erosion development in study area. Therefore, targeted measures and control strategies should be designed based on a comprehensive assessment of terrain factors and landscape pattern indicators to mitigate gully erosion risks. In the future, based on obtaining more three-dimensional data of gullies, empirical coefficient equations should be constructed using gully area and length as independent variables to predict gully volume. This will help identify the main factors influencing sediment and organic matter loss caused by gully erosion in black soil region, and provide technical support for improving the predictive capabilities of gully erosion risks and developing more rational prevention and control strategies.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106434"},"PeriodicalIF":6.1,"publicationDate":"2024-12-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142889230","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The application of amendments improves properties of salt-affected soils across China 改良剂的应用改善了中国盐渍土壤的性质
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-20 DOI: 10.1016/j.still.2024.106431
Guangzhi Huang , Baishun Liu , Xiaotong Jiang , Yanping Liang , Jinghui Cai , Lihua Huang
Soil salinization is a major threat to global arable productivity. Chemical amendments are widely used to improve salt-affected soils and have been proven to be effective. However, the effectiveness of amendments varies across different regions and depends on field management practices. To quantify the improvement effects of different amendments on salt-affected soils and how amendment application affects plant productivity and soil properties, we compiled 2061 pairs of data from 92 studies about amendments across China to conduct a meta-analysis. We found that amendments application improved soil quality by reducing soil pH, electrical conductivity (EC), and exchangeable sodium percentage (ESP) with 3.9 %, 18.1 %, and 43.4 %, and improved soil nutrients by increasing soil organic matter (SOM), total nitrogen (TN), available nitrogen (AN), available phosphorus (AP), and available potassium (AK) with 33.6 %, 37.7 %, 35.0 %, 55.3 %, and 32.3 %, and subsequently increased plant emergence rate and yield with 16.2 % and 52.2 % regardless of amendment types, respectively. Specifically, applying mixed amendments led to a significant reduction in soil EC by 33.6 %, whereas the application of inorganic compound decreased soil EC by 8.6 %. Furthermore, biochar application significantly increased SOM by 58.4 % and TN by 46.2 %, while gypsum application increased SOM and TN with only 20.9 % and 17.4 %, respectively. Field management, soil properties, and climate all significantly affected the improvement effect after amendments application. The effects of improving salt-affected soil were strongly correlated with the amount and duration of amendments application, followed by the initial soil salinity and alkalinity. Our findings indicated that the selection of soil amendments should consider not only their quantity but also factors such as cost, the longevity of their effects, and environmental safety.
土壤盐碱化是全球耕地生产力的主要威胁。化学改良剂被广泛用于改善盐渍土壤,并已被证明是有效的。然而,修订的有效性因区域而异,并取决于实地管理做法。为了量化不同改良剂对盐渍土壤的改良效果,以及改良剂施用对植物生产力和土壤性质的影响,我们收集了来自中国各地92项改良剂研究的2061对数据进行了荟萃分析。结果表明,施用改良剂可通过降低土壤pH值、电导率(EC)和交换性钠百分比(ESP)(分别为3.9 %、18.1 %和43.4 %)改善土壤质量,通过提高土壤有机质(SOM)、全氮(TN)、速效氮(AN)、速效磷(AP)和速效钾(AK)(分别为33.6 %、37.7 %、35.0 %、55.3 %和32.3 %)改善土壤养分。在不同改良类型下,均能提高植株出苗率16.2 %和产量52.2 %。具体来说,施用混合改剂剂导致土壤EC显著减少33.6% %,而施用无机化合物则使土壤EC减少8.6% %。施用生物炭可显著提高土壤有机质58.4% %和全氮46.2% %,而施用石膏可显著提高土壤有机质20.9% %和全氮17.4% %。施用改良剂后,田间管理、土壤性质和气候对改良效果均有显著影响。改良盐渍化土壤的效果与改良剂施用量和施用时间密切相关,其次是土壤初始盐度和碱度。研究结果表明,土壤改良剂的选择不仅要考虑其数量,还要考虑其成本、效果持续时间和环境安全性等因素。
{"title":"The application of amendments improves properties of salt-affected soils across China","authors":"Guangzhi Huang ,&nbsp;Baishun Liu ,&nbsp;Xiaotong Jiang ,&nbsp;Yanping Liang ,&nbsp;Jinghui Cai ,&nbsp;Lihua Huang","doi":"10.1016/j.still.2024.106431","DOIUrl":"10.1016/j.still.2024.106431","url":null,"abstract":"<div><div>Soil salinization is a major threat to global arable productivity. Chemical amendments are widely used to improve salt-affected soils and have been proven to be effective. However, the effectiveness of amendments varies across different regions and depends on field management practices. To quantify the improvement effects of different amendments on salt-affected soils and how amendment application affects plant productivity and soil properties, we compiled 2061 pairs of data from 92 studies about amendments across China to conduct a meta-analysis. We found that amendments application improved soil quality by reducing soil pH, electrical conductivity (EC), and exchangeable sodium percentage (ESP) with 3.9 %, 18.1 %, and 43.4 %, and improved soil nutrients by increasing soil organic matter (SOM), total nitrogen (TN), available nitrogen (AN), available phosphorus (AP), and available potassium (AK) with 33.6 %, 37.7 %, 35.0 %, 55.3 %, and 32.3 %, and subsequently increased plant emergence rate and yield with 16.2 % and 52.2 % regardless of amendment types, respectively. Specifically, applying mixed amendments led to a significant reduction in soil EC by 33.6 %, whereas the application of inorganic compound decreased soil EC by 8.6 %. Furthermore, biochar application significantly increased SOM by 58.4 % and TN by 46.2 %, while gypsum application increased SOM and TN with only 20.9 % and 17.4 %, respectively. Field management, soil properties, and climate all significantly affected the improvement effect after amendments application. The effects of improving salt-affected soil were strongly correlated with the amount and duration of amendments application, followed by the initial soil salinity and alkalinity. Our findings indicated that the selection of soil amendments should consider not only their quantity but also factors such as cost, the longevity of their effects, and environmental safety.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106431"},"PeriodicalIF":6.1,"publicationDate":"2024-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142867542","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Reclamation leads to loss of soil organic carbon and molecular complexity: Evidence from natural to reclaimed wetlands 开垦导致土壤有机碳和分子复杂性的损失:从自然湿地到开垦湿地的证据
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-20 DOI: 10.1016/j.still.2024.106436
Xiaolei Yin , Xiaofei Yu , Lei Qin , Ming Jiang , Xianguo Lu , Yuanchun Zou
The molecular diversity of soil organic matter (SOM) is recognised as a key factor influencing soil organic carbon (SOC) accumulation, and the molecular diversity of SOM may change as SOC content changes during land use change. However, the relationship between SOM molecular diversity and SOC before and after natural wetland reclamation remains unclear. Here, we selected seven groups of natural wetland–reclaimed wetlands for spatially paired sampling. SOM molecular diversity was assessed using pyrolysis–gas chromatography–mass spectrometry (py-GC/MS), and factors driving changes in SOM molecular diversity (including microbial community characteristics, enzyme activities, carbon mineralisation rate and soil environmental factors) were investigated. The results showed that molecular diversity (Shannon diversity, Richness) tended to increase with increasing organic carbon content in both wetland and paddy soils. And the soil mineralisation rate decreased with the increase of molecular diversity. This suggests that the relationship between molecular diversity and organic carbon content is not decoupled, even in anaerobic or cyclic anaerobic environments. Therefore, the molecular diversity of soil organic matter can be used as an indicator of the sustainability of soil carbon pools. Microbial biomass and enzyme activity characteristics were important factors influencing soil carbon dynamics and molecular diversity. Molecular diversity decreases with a loss of soil organic carbon after wetland reclamation. Compared to those in natural wetlands, the relative proportions of both aliphatic and alkyl compounds decreased, and the relative proportions of nitrogenous compounds increased in paddy field soils. In addition, the rate of soil carbon mineralisation increases despite the presence of a greater proportion of recalcitrant carbon (phenols and aromatics) in paddy soils. Our results also suggest a positive role for molecular diversity in suppressing soil mineralization rates. Our study provides a molecular diversity-based perspective for understanding wetland soil organic carbon dynamics under the influence of reclamation.
土壤有机质(SOM)分子多样性是影响土壤有机碳(SOC)积累的关键因素,在土地利用变化过程中,土壤有机质(SOM)分子多样性可能随着土壤有机碳含量的变化而变化。然而,湿地自然开垦前后SOM分子多样性与有机碳的关系尚不清楚。本文选取7组天然湿地-人工湿地进行空间配对采样。采用热解-气相色谱-质谱法(pygc /MS)对土壤有机质分子多样性进行了评价,并对土壤有机质分子多样性变化的驱动因素(包括微生物群落特征、酶活性、碳矿化率和土壤环境因素)进行了研究。结果表明,随着有机碳含量的增加,湿地和水稻土的分子多样性(Shannon多样性、丰富度)均呈增加趋势。土壤矿化率随分子多样性的增加而降低。这表明,即使在厌氧或循环厌氧环境中,分子多样性和有机碳含量之间的关系也不是解耦的。因此,土壤有机质分子多样性可以作为土壤碳库可持续性的一个指标。微生物生物量和酶活性特征是影响土壤碳动态和分子多样性的重要因素。湿地复垦后,分子多样性随着土壤有机碳的减少而降低。与天然湿地相比,水田土壤中脂肪族化合物和烷基化合物的相对比例均降低,氮化合物的相对比例升高。此外,尽管水稻土中存在更大比例的顽固性碳(酚类和芳烃),但土壤碳矿化率仍在增加。我们的研究结果还表明,分子多样性在抑制土壤矿化率方面具有积极作用。本研究为理解开垦影响下湿地土壤有机碳动态提供了基于分子多样性的视角。
{"title":"Reclamation leads to loss of soil organic carbon and molecular complexity: Evidence from natural to reclaimed wetlands","authors":"Xiaolei Yin ,&nbsp;Xiaofei Yu ,&nbsp;Lei Qin ,&nbsp;Ming Jiang ,&nbsp;Xianguo Lu ,&nbsp;Yuanchun Zou","doi":"10.1016/j.still.2024.106436","DOIUrl":"10.1016/j.still.2024.106436","url":null,"abstract":"<div><div>The molecular diversity of soil organic matter (SOM) is recognised as a key factor influencing soil organic carbon (SOC) accumulation, and the molecular diversity of SOM may change as SOC content changes during land use change. However, the relationship between SOM molecular diversity and SOC before and after natural wetland reclamation remains unclear. Here, we selected seven groups of natural wetland–reclaimed wetlands for spatially paired sampling. SOM molecular diversity was assessed using pyrolysis–gas chromatography–mass spectrometry (py-GC/MS), and factors driving changes in SOM molecular diversity (including microbial community characteristics, enzyme activities, carbon mineralisation rate and soil environmental factors) were investigated. The results showed that molecular diversity (Shannon diversity, Richness) tended to increase with increasing organic carbon content in both wetland and paddy soils. And the soil mineralisation rate decreased with the increase of molecular diversity. This suggests that the relationship between molecular diversity and organic carbon content is not decoupled, even in anaerobic or cyclic anaerobic environments. Therefore, the molecular diversity of soil organic matter can be used as an indicator of the sustainability of soil carbon pools. Microbial biomass and enzyme activity characteristics were important factors influencing soil carbon dynamics and molecular diversity. Molecular diversity decreases with a loss of soil organic carbon after wetland reclamation. Compared to those in natural wetlands, the relative proportions of both aliphatic and alkyl compounds decreased, and the relative proportions of nitrogenous compounds increased in paddy field soils. In addition, the rate of soil carbon mineralisation increases despite the presence of a greater proportion of recalcitrant carbon (phenols and aromatics) in paddy soils. Our results also suggest a positive role for molecular diversity in suppressing soil mineralization rates. Our study provides a molecular diversity-based perspective for understanding wetland soil organic carbon dynamics under the influence of reclamation.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106436"},"PeriodicalIF":6.1,"publicationDate":"2024-12-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142867511","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Long-term rice–crayfish coculture increases plant lignin but not microbial necromass contribution to soil organic carbon 长期水稻-小龙虾共培养增加了植物木质素,但没有增加微生物坏死团对土壤有机碳的贡献
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-19 DOI: 10.1016/j.still.2024.106424
Yao Guo , Quanyi Hu , Tianqi Liu , Yunfeng Du , Chengfang Li , Xuelin Zhang , Juan Liu , Cougui Cao
Rice–crayfish coculture (RC) has emerged as a transformative agricultural practice in China, significantly influencing soil microorganisms and enhancing soil organic carbon (SOC) accumulation. However, the contribution of plant residues and microbial necromass to the increased SOC within RC systems remains uncertain. This study aimed to investigate phospholipid fatty acids (PLFAs), microbial necromass C (MNC, with amino sugars as biomarkers), plant-derived C (VSC, with lignin phenols as biomarkers) levels, along with soil properties across conventional rice monoculture (RM) and RC systems of 5-, 10-, and 15-yr durations (RC5, RC10, and RC15, respectively). The results showed that long-term RC fields exhibited stronger aggregation, higher soil nutrient levels, organically complexed Fe oxides (Fep), and lower bulk density and oxidation–reduction potential than those with RM. The SOC levels were significantly higher in RC10 and RC15 than in RM, by 31.8 % and 37.2 %, respectively. Moreover, RC significantly reduced the levels of bacterial (25.3–35.4 %) and fungal (19.5–34.7 %) PLFAs compared with RM, with RC10 exhibiting the lowest levels. With RC duration increasing to 10–15 years, MNC and VSC were respectively higher by 12.4–25.3 % and 48.8–72.4 % than those in RM. Specifically, fungal necromass C, as well as vanillyl- and syringyl-type phenols, showed the most pronounced enhancements. Concurrently, the contribution of VSC to SOC (12.4–25.3 %) significantly increased in the 10 −15-yr RC period compared with RM, whereas MNC decreased proportionally (17.5–18.5 %). SOC and Fep were the primary factors regulating the contribution of MNC to SOC, whereas the contribution of VSC to SOC was mainly influenced by soil aggregation. Thus, long-term RC improved soil C sequestration primarily by increasing the contribution of plant-derived C rather than that of microbe-derived C. However, the findings of this study indicated that long-term RC might limit microbial biomass, thereby raising concerns about the long-term sustainability of microbial communities in these systems.
水稻-小龙虾共养(RC)已成为中国一种变革性的农业实践,显著影响了土壤微生物,提高了土壤有机碳(SOC)的积累。然而,植物残体和微生物坏死块对土壤有机碳增加的贡献仍不确定。本研究旨在研究5年、10年和15年(分别为RC5、RC10和RC15)的传统水稻单栽培(RM)和RC系统中磷脂脂肪酸(PLFAs)、微生物坏死团C (MNC,以氨基糖为生物标志物)、植物源性C (VSC,以木质素酚为生物标志物)水平以及土壤特性。结果表明,长期施用RC的土壤团聚性较强,土壤养分水平较高,铁氧化物有机络合,容重和氧化还原电位较低。RC10和RC15的SOC水平显著高于RM,分别提高了31.8% %和37.2% %。此外,与RM相比,RC显著降低了细菌PLFAs(25.3-35.4 %)和真菌PLFAs(19.5-34.7 %)的水平,其中RC10的水平最低。随着RC龄期的增加,MNC和VSC分别比RM高12.4 ~ 25.3 %和48.8 ~ 72.4 %。具体来说,真菌坏死团C,以及香草基和丁香基型酚,表现出最明显的增强。与此同时,与RM相比,VSC对SOC的贡献在10 −15年的RC期间显著增加(12.4-25.3 %),而MNC则呈比例下降(17.5-18.5 %)。土壤有机碳和Fep是影响土壤有机碳贡献的主要因子,而VSC对土壤有机碳的贡献主要受土壤团聚体的影响。因此,长期RC主要通过增加植物来源的C而不是微生物来源的C来改善土壤碳固存。然而,本研究的结果表明,长期RC可能会限制微生物生物量,从而引起对这些系统中微生物群落长期可持续性的关注。
{"title":"Long-term rice–crayfish coculture increases plant lignin but not microbial necromass contribution to soil organic carbon","authors":"Yao Guo ,&nbsp;Quanyi Hu ,&nbsp;Tianqi Liu ,&nbsp;Yunfeng Du ,&nbsp;Chengfang Li ,&nbsp;Xuelin Zhang ,&nbsp;Juan Liu ,&nbsp;Cougui Cao","doi":"10.1016/j.still.2024.106424","DOIUrl":"10.1016/j.still.2024.106424","url":null,"abstract":"<div><div>Rice–crayfish coculture (RC) has emerged as a transformative agricultural practice in China, significantly influencing soil microorganisms and enhancing soil organic carbon (SOC) accumulation. However, the contribution of plant residues and microbial necromass to the increased SOC within RC systems remains uncertain. This study aimed to investigate phospholipid fatty acids (PLFAs), microbial necromass C (MNC, with amino sugars as biomarkers), plant-derived C (VSC, with lignin phenols as biomarkers) levels, along with soil properties across conventional rice monoculture (RM) and RC systems of 5-, 10-, and 15-yr durations (RC5, RC10, and RC15, respectively). The results showed that long-term RC fields exhibited stronger aggregation, higher soil nutrient levels, organically complexed Fe oxides (Fe<sub>p</sub>), and lower bulk density and oxidation–reduction potential than those with RM. The SOC levels were significantly higher in RC10 and RC15 than in RM, by 31.8 % and 37.2 %, respectively. Moreover, RC significantly reduced the levels of bacterial (25.3–35.4 %) and fungal (19.5–34.7 %) PLFAs compared with RM, with RC10 exhibiting the lowest levels. With RC duration increasing to 10–15 years, MNC and VSC were respectively higher by 12.4–25.3 % and 48.8–72.4 % than those in RM. Specifically, fungal necromass C, as well as vanillyl- and syringyl-type phenols, showed the most pronounced enhancements. Concurrently, the contribution of VSC to SOC (12.4–25.3 %) significantly increased in the 10 −15-yr RC period compared with RM, whereas MNC decreased proportionally (17.5–18.5 %). SOC and Fe<sub>p</sub> were the primary factors regulating the contribution of MNC to SOC, whereas the contribution of VSC to SOC was mainly influenced by soil aggregation. Thus, long-term RC improved soil C sequestration primarily by increasing the contribution of plant-derived C rather than that of microbe-derived C. However, the findings of this study indicated that long-term RC might limit microbial biomass, thereby raising concerns about the long-term sustainability of microbial communities in these systems.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106424"},"PeriodicalIF":6.1,"publicationDate":"2024-12-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142867509","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Soil physical properties and water dynamics under contrasting management regimes at the Morrow Plots 莫罗地块不同管理制度下的土壤物理特性和水动力学
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-19 DOI: 10.1016/j.still.2024.106422
Peter B. Obour , Yushu Xia , Carmen M. Ugarte , Tony E. Grift , Michelle M. Wander
This study investigated changes in soil physical quality and water dynamics arising from continuous cropping at the Morrow Plots, the oldest agricultural experiment in North America. The objectives were to examine the effects of continuous cultivation on soil water retention and determine the optimum water content for tillage (θOPT) in a prime agricultural soil. Soil samples collected at 0–5, 5–10, and 10–15 cm depths were used to measure bulk density and water retention using the HyProp 2 and WP4-T Dewpoint Potentiometer. Soil organic carbon (SOC) and soil penetration resistance (PR) were measured to a depth of 15 cm. The soil water retention data were fitted with the Dexter double exponential and van Genuchten models. Neither model consistently fitted all the water retention data across the different management practices. The corn-oat-hay (COH) rotation generally reduced soil bulk density within the 0–15 cm depth by an average of 9 % and PR by 21 % compared to the continuous corn (CC) treatment. The COH rotation slightly increased topsoil water-holding capacity (0–15 cm), although trends varied with fertility regimes. The θOPT for the COH and CC estimated by the van Genuchten model was generally wetter than the water content at field capacity (θFC). In contrast, the θOPT estimated by the Dexter model was slightly drier than θFC. Despite limitations due to the lack of true replicates and the small sample size at the Morrow Plots, this research underscores the long-term impact of crop rotation on soil hydraulic properties in prime agricultural soils.
这项研究调查了北美最古老的农业试验莫罗地块连作引起的土壤物理质量和水动力学的变化。目的是检查连续耕作对土壤保水的影响,并确定在优质农业土壤中耕作的最佳含水量(θOPT)。使用HyProp 2和WP4-T露点电位器测量0-5、5-10和10-15 cm深度的土壤样品的容重和保水率。测定土壤有机碳(SOC)和土壤穿透阻力(PR),深度为15 cm。土壤保水数据采用Dexter双指数模型和van Genuchten模型进行拟合。两个模型都不能一致地拟合不同管理实践中的所有保水性数据。与连续玉米(CC)处理相比,玉米-燕麦-干草(COH)轮作一般使0-15 cm深度内的土壤容重平均降低9 %,PR平均降低21 %。COH轮作略微增加了表土持水能力(0-15 cm),尽管趋势因肥力制度而异。van Genuchten模型估计的COH和CC的θOPT通常比现场容量含水量(θFC)更湿。相比之下,Dexter模型估计的θOPT比θFC略干。尽管由于缺乏真正的重复和莫罗地块的小样本量而受到限制,但该研究强调了作物轮作对优质农业土壤土壤水力特性的长期影响。
{"title":"Soil physical properties and water dynamics under contrasting management regimes at the Morrow Plots","authors":"Peter B. Obour ,&nbsp;Yushu Xia ,&nbsp;Carmen M. Ugarte ,&nbsp;Tony E. Grift ,&nbsp;Michelle M. Wander","doi":"10.1016/j.still.2024.106422","DOIUrl":"10.1016/j.still.2024.106422","url":null,"abstract":"<div><div>This study investigated changes in soil physical quality and water dynamics arising from continuous cropping at the Morrow Plots, the oldest agricultural experiment in North America. The objectives were to examine the effects of continuous cultivation on soil water retention and determine the optimum water content for tillage (<em>θ</em><sub>OPT</sub>) in a prime agricultural soil. Soil samples collected at 0–5, 5–10, and 10–15 cm depths were used to measure bulk density and water retention using the HyProp 2 and WP4-T Dewpoint Potentiometer. Soil organic carbon (SOC) and soil penetration resistance (PR) were measured to a depth of 15 cm. The soil water retention data were fitted with the Dexter double exponential and van Genuchten models. Neither model consistently fitted all the water retention data across the different management practices. The corn-oat-hay (COH) rotation generally reduced soil bulk density within the 0–15 cm depth by an average of 9 % and PR by 21 % compared to the continuous corn (CC) treatment. The COH rotation slightly increased topsoil water-holding capacity (0–15 cm), although trends varied with fertility regimes. The <em>θ</em><sub>OPT</sub> for the COH and CC estimated by the van Genuchten model was generally wetter than the water content at field capacity (<em>θ</em><sub>FC</sub><em>)</em>. In contrast, the <em>θ</em><sub>OPT</sub> estimated by the Dexter model was slightly drier than <em>θ</em><sub>FC</sub>. Despite limitations due to the lack of true replicates and the small sample size at the Morrow Plots, this research underscores the long-term impact of crop rotation on soil hydraulic properties in prime agricultural soils.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"248 ","pages":"Article 106422"},"PeriodicalIF":6.1,"publicationDate":"2024-12-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142867547","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":1,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"OA","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
期刊
Soil & Tillage Research
全部 Acc. Chem. Res. ACS Applied Bio Materials ACS Appl. Electron. Mater. ACS Appl. Energy Mater. ACS Appl. Mater. Interfaces ACS Appl. Nano Mater. ACS Appl. Polym. Mater. ACS BIOMATER-SCI ENG ACS Catal. ACS Cent. Sci. ACS Chem. Biol. ACS Chemical Health & Safety ACS Chem. Neurosci. ACS Comb. Sci. ACS Earth Space Chem. ACS Energy Lett. ACS Infect. Dis. ACS Macro Lett. ACS Mater. Lett. ACS Med. Chem. Lett. ACS Nano ACS Omega ACS Photonics ACS Sens. ACS Sustainable Chem. Eng. ACS Synth. Biol. Anal. Chem. BIOCHEMISTRY-US Bioconjugate Chem. BIOMACROMOLECULES Chem. Res. Toxicol. Chem. Rev. Chem. Mater. CRYST GROWTH DES ENERG FUEL Environ. Sci. Technol. Environ. Sci. Technol. Lett. Eur. J. Inorg. Chem. IND ENG CHEM RES Inorg. Chem. J. Agric. Food. Chem. J. Chem. Eng. Data J. Chem. Educ. J. Chem. Inf. Model. J. Chem. Theory Comput. J. Med. Chem. J. Nat. Prod. J PROTEOME RES J. Am. Chem. Soc. LANGMUIR MACROMOLECULES Mol. Pharmaceutics Nano Lett. Org. Lett. ORG PROCESS RES DEV ORGANOMETALLICS J. Org. Chem. J. Phys. Chem. J. Phys. Chem. A J. Phys. Chem. B J. Phys. Chem. C J. Phys. Chem. Lett. Analyst Anal. Methods Biomater. Sci. Catal. Sci. Technol. Chem. Commun. Chem. Soc. Rev. CHEM EDUC RES PRACT CRYSTENGCOMM Dalton Trans. Energy Environ. Sci. ENVIRON SCI-NANO ENVIRON SCI-PROC IMP ENVIRON SCI-WAT RES Faraday Discuss. Food Funct. Green Chem. Inorg. Chem. Front. Integr. Biol. J. Anal. At. Spectrom. J. Mater. Chem. A J. Mater. Chem. B J. Mater. Chem. C Lab Chip Mater. Chem. Front. Mater. Horiz. MEDCHEMCOMM Metallomics Mol. Biosyst. Mol. Syst. Des. Eng. Nanoscale Nanoscale Horiz. Nat. Prod. Rep. New J. Chem. Org. Biomol. Chem. Org. Chem. Front. PHOTOCH PHOTOBIO SCI PCCP Polym. Chem.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1