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Silicon reduces cadmium accumulation in Moso bamboo (Phyllostachys edulis) root cell sap by sequestering cadmium in hemicellulose 1 硅通过在半纤维素中固存镉,减少毛竹根液中镉的积累
IF 5.2 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-01 DOI: 10.1016/j.pedsph.2023.07.015
Yuzhen CHANG , Fan YANG , Chaofeng YANG , Yiting ZHENG , Xianyu PAN , Shanshan MA , Haibao JI , Ji Feng SHAO
Moso bamboo is one of the most important economic bamboo species in China, but cadmium (Cd) pollution has become a potential threat of its sustainable development. Silicon (Si) reduces Cd accumulation in many plant species. However, the exact mechanisms of this effect in Moso bamboo are still poorly understood. Here, we investigated the effect of Si on Cd accumulation in Moso bamboo in terms of Cd concentration in roots, Cd cellular and subcellular distribution, root cell morphology, and gene expression. Seedlings (ten days old) were exposed to different concentrations of Cd (0, 1, 5, and 50 μmol L-1) in a 0.5 mmol L-1 CaCl2 solution treated with (+Si) and without (-Si) 1 mmol L-1 Si (as silicic acid) for two days. The effect of Si on the alleviation of Cd-induced inhibition of root elongation was not obvious, but Si could significantly reduce Cd accumulation in roots at all tested Cd concentrations (1, 5, and 50 μmol L-1). Cadmium was localized in all cells of roots, but Si application altered the Cd distribution from all cells to distal side of exodermis cells in roots. Semi-quantitative determination of Cd using energy-dispersive X-rays revealed higher Cd concentrations in exodermis, but lower concentrations in the stele when Si was applied. However, Si increased Cd accumulation in root cell wall, but decreased it in cell sap. Moreover, more than 70% of Cd and Si were found in hemicellulose 1 of the cell wall. These results suggested that Si reduced Cd accumulation by sequestering Cd in hemicellulose 1 in the root cell wall at the subcellular level and retaining most of the Cd in the root exodermis at the cellular level in Moso bamboo under short-term Si application.
毛竹是中国最重要的经济竹种之一,但镉污染已成为其可持续发展的潜在威胁。硅(Si)在许多植物物种中减少镉的积累。然而,这种作用在毛竹中的确切机制仍然知之甚少。本研究从根系Cd浓度、Cd细胞和亚细胞分布、根细胞形态和基因表达等方面研究了Si对毛梭竹Cd积累的影响。将10天大的幼苗在0.5 mmol L-1 CaCl2溶液中暴露于不同浓度的Cd(0、1、5和50 μmol L-1), CaCl2溶液中添加(+Si)和不添加(-Si) 1 mmol L-1 Si(硅酸),处理2天。在Cd浓度(1、5和50 μmol L-1)下,Si对Cd诱导的根伸长抑制的缓解作用不明显,但Si能显著降低根中Cd的积累。镉定位于根的所有细胞,但施硅改变了镉从根的所有细胞向远端外表皮细胞的分布。利用能量色散x射线对Cd进行半定量测定,结果显示外表皮中Cd浓度较高,但在石柱中Si浓度较低。而Si增加了根细胞壁中Cd的积累,但降低了根汁液中Cd的积累,并且在细胞壁的半纤维素1中发现了70%以上的Cd和Si。这些结果表明,在短期施用硅的情况下,硅通过在亚细胞水平上将镉吸附在毛竹根细胞壁的半纤维素1中,在细胞水平上将大部分镉保留在根外表皮中,从而减少了镉的积累。
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引用次数: 0
Microbial genes for degrading plant-derived carbon are a key factor affecting soil respiration and temperature sensitivity in plateau peatlands 降解植物碳的微生物基因是影响高原泥炭地土壤呼吸作用和温度敏感性的关键因素
IF 5.2 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-01 DOI: 10.1016/j.pedsph.2024.07.003
Wei JIANG , Mingyao XIONG , Shuzhen ZOU , Di KANG
Peatlands on the southwestern plateau of China are important carbon sinks for high-altitude terrestrial ecosystems in Asia. However, the specific microecological mechanism responsible for alterations in carbon processes in this region due to the simultaneous impacts of global warming and drought has not been fully elucidated. Investigating this mechanism will improve our understanding of carbon cycle feedback in peatland ecosystems, as it is affected by changes in hydrology and temperature, especially in vulnerable habitats. This study examined the influence of soil carbon decomposition functional microorganisms on soil respiration and temperature sensitivity (expressed as Q10) in high-elevation peatlands using field investigations, simulated warming experiments, and metagenomic sequencing. We found that hydrothermal conditions had a significant effect on soil respiration, leading to an increase in cumulative soil respiration as soil moisture and temperature increased. Soil moisture affected soil respiration and soil organic carbon mainly through soil microorganisms, with a predominance of carbon-decomposing genes. We found that genes regulating the decomposition of plant-derived carbon such as cellulose and lignin were the critical factor influencing Q10 in peatlands. Genes involved in cellulose and lignin decomposition showed a significant positive correlation with Q10 (P < 0.05), while genes involved in hemicellulose decomposition showed a significant negative correlation with Q10 (P < 0.05). Specifically, genes such as ACO, xylF, and hpaE, which are involved in lignin decomposition, and glgB, which is responsible for cellulose decomposition, showed significant positive correlations (P < 0.05) with Q10. Conversely, the gene uxaC, involved in the decomposition of hemicellulose, showed a significant negative correlation (P < 0.05) with Q10. Finally, we analyzed the relevant carbon metabolic pathways and found that although they were affected by water, they were not significantly related to Q10. In short, this research highlights the importance of microorganisms with genes for decomposing plant-derived carbon in influencing carbon emissions in plateau peatlands during periods of warming.
中国西南高原泥炭地是亚洲高海拔陆地生态系统的重要碳汇。然而,由于全球变暖和干旱的同时影响,导致该地区碳过程变化的具体微生态机制尚未完全阐明。研究这一机制将提高我们对泥炭地生态系统中碳循环反馈的理解,因为它受水文和温度变化的影响,特别是在脆弱的栖息地。采用野外调查、模拟增温实验和宏基因组测序等方法,研究了高海拔泥炭地土壤碳分解功能微生物对土壤呼吸和温度敏感性(表达为Q10)的影响。热液条件对土壤呼吸有显著影响,随着土壤湿度和温度的升高,累积土壤呼吸增加。土壤水分主要通过土壤微生物影响土壤呼吸和土壤有机碳,且以分解碳基因为主。我们发现,调控植物源碳(如纤维素和木质素)分解的基因是影响泥炭地Q10的关键因素。参与纤维素和木质素分解的基因与Q10呈显著正相关(P <;0.05),而参与半纤维素分解的基因与Q10呈显著负相关(P <;0.05)。具体而言,参与木质素分解的ACO、xylF和hpaE等基因与负责纤维素分解的glgB呈显著正相关(P <;0.05)。相反,参与半纤维素分解的uxaC基因则表现出显著的负相关(P <;0.05)。最后,我们分析了相关的碳代谢途径,发现它们虽然受到水分的影响,但与辅酶Q10的相关性不显著。简而言之,本研究强调了具有分解植物源碳基因的微生物在变暖期间影响高原泥炭地碳排放的重要性。
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引用次数: 0
Role of nosZ I-carrying microorganisms in regulating nitrous oxide reduction during forest conversion: A comparison of plantations and a secondary forest in subtropical soils 森林转化过程中携带nosZ i的微生物在调节氧化亚氮还原中的作用:亚热带土壤人工林与次生林的比较
IF 5.2 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-12-01 DOI: 10.1016/j.pedsph.2023.09.006
Milin DENG , Guiping YE , Hang-Wei HU , Chao XU , Ping YANG , Yong ZHENG , Jupei SHEN , Shengsheng JIN , Ji-Zheng HE , Yongxin LIN
The conversion of natural forests in subtropical regions to plantations or secondary forests has resulted in alterations in soil variables, microbial communities, and microbially mediated processes, including nitrous oxide (N2O) emissions. However, how forest conversion influences soil N2O reduction and the abundance and community structure of N2O-reducing microorganisms remains unclear. Here, we investigated the impact of converting natural forests to a secondary forest and Cunninghamia lanceolata and Pinus massoniana plantations on the abundance and community structure of N2O-reducing microorganisms in both bulk soils and soil aggregates. Compared with the secondary forest, plantations had higher soil pH and available phosphorus and moisture contents, lower soil NH4+ content, but similar aggregate sizes. Compared with the secondary forest, the conversion of natural forest to plantations resulted in significantly higher soil N2O reduction rate and increased abundances of nosZ I and nosZ II genes in bulk soils and soil aggregates. The abundance of nosZ I was higher than that of nosZ II in all tested soils and had a stronger association with N2O reduction rate, suggesting the greater role of nosZ I-carrying microorganisms in N2O consumption. Forest conversion had a greater impact on the community composition of nosZ I than nosZ II, mainly by increasing the relative abundances of alpha- and beta-Proteobacteria, while decreasing gamma-Proteobacteria. However, nosZ II-carrying microorganisms were exclusively dominated by Gemmatimonadetes and less affected by forest conversion. Taken together, our findings significantly contribute to our understanding of the eco-physiological characteristics of N2O-reducing microorganisms and highlight the importance of nosZ I-carrying microorganisms in N2O consumption in subtropical forest soils.
亚热带地区天然林向人工林或次生林的转变导致土壤变量、微生物群落和微生物介导的过程(包括氧化亚氮(N2O)排放)发生变化。然而,森林转换如何影响土壤N2O还原以及N2O还原微生物的丰度和群落结构尚不清楚。本文研究了天然林向次生林、杉木人工林和马尾松人工林对土壤和土壤团聚体中n2o还原微生物丰度和群落结构的影响。与次生林相比,人工林土壤pH、速效磷和水分含量较高,NH4+含量较低,但团聚体粒径相近。与次生林相比,天然林还林后土壤N2O还原速率显著提高,土壤体和团聚体中nosZ I和nosZ II基因丰度显著增加。nosZ I丰度均高于nosZ II,且与N2O还原速率的相关性更强,说明携带nosZ I的微生物在N2O消耗中的作用更大。森林转换对nosZ I群落组成的影响大于nosZ II,主要是通过增加α -和β -变形菌门的相对丰度,而降低γ -变形菌门的相对丰度。而携带nosZ ii的微生物主要以Gemmatimonadetes类为主,受森林转化的影响较小。综上所述,我们的研究结果有助于我们了解N2O还原微生物的生态生理特征,并强调了携带nosZ i的微生物在亚热带森林土壤N2O消耗中的重要性。
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引用次数: 0
Spatial-temporal simulation and prediction of root zone soil moisture based on Hydrus-1D and CNN-LSTM-attention models in Yutian Oasis, southern Xinjiang, China 基于Hydrus-1D和CNN-LSTM-attention模型的南疆玉田绿洲根区土壤水分时空模拟与预测
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-10-15 DOI: 10.1016/j.pedsph.2024.10.008
Xiaobo LÜ , Ilyas NURMEMET , Sentian XIAO , Jing ZHAO , Xinru YU , Yilizhati AILI , Shiqin LI
Root zone soil moisture (RZSM) plays a critical role in land-atmosphere hydrological cycles and serves as the primary water source for vegetation growth. However, the correlations between RZSM and its associated variables, including surface soil moisture (SSM), often exhibit nonlinearities that are challenging to identify and quantify using conventional statistical techniques. Therefore, this study presents a hybrid convolutional neural network (CNN)-long short-term memory neural network (LSTM)-attention (CLA) model for predicting RZSM. Owing to the scarcity of soil moisture (SM) observation data, the physical model Hydrus-1D was employed to simulate a comprehensive dataset of spatial-temporal SM. Meteorological data and moderate resolution imaging spectroradiometer vegetation characterization parameters were used as predictor variables for the training and validation of the CLA model. The results of the CLA model for SM prediction in the root zone were significantly enhanced compared with those of the traditional LSTM and CNN-LSTM models. This was particularly notable at the depth of 80–100 cm, where the fitness (R2) reached nearly 0.929 8. Moreover, the root mean square error of the CLA model was reduced by 49% and 57% compared with those of the LSTM and CNN-LSTM models, respectively. This study demonstrates that the integration of physical modeling and deep learning methods provides a more comprehensive and accurate understanding of spatial-temporal SM variations in the root zone.
根区土壤水分在陆地-大气水循环中起着至关重要的作用,是植被生长的主要水源。然而,RZSM与其相关变量(包括表层土壤湿度(SSM))之间的相关性通常表现出非线性,这对使用传统统计技术识别和量化具有挑战性。因此,本研究提出了一种混合卷积神经网络(CNN)长短期记忆神经网络(LSTM)-注意(CLA)预测RZSM的模型。由于土壤湿度观测数据的缺乏,采用Hydrus-1D物理模型模拟了一个综合的土壤湿度时空数据集。利用气象数据和中分辨率成像光谱辐射计植被特征参数作为预测变量,对CLA模型进行训练和验证。与传统LSTM和CNN-LSTM模型相比,CLA模型对根区SM的预测结果显著增强。这在80 ~ 100 cm深度尤为显著,适应度(R2)接近0.929 8。与LSTM和CNN-LSTM模型相比,CLA模型的均方根误差分别减小了49%和57%。该研究表明,物理建模与深度学习方法的结合可以更全面、准确地了解根区SM的时空变化。
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引用次数: 0
Efficiency-enhancing methods for predicting nitrogen mineralization characteristics in paddy soils using soil properties and rapid soil extractions 利用土壤特性和快速土壤提取技术预测水稻土氮矿化特征的高效方法
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-10-04 DOI: 10.1016/j.pedsph.2024.10.001
Yujuan LIU , Yuqi CHEN , Xiuyun LIU , Siyuan CAI , Jiahui YUAN , Lingying XU , Yu WANG , Xu ZHAO , Xiaoyuan YAN
Soil mineralized nitrogen (N) is a vital component of soil N supply capacity and an important N source for rice growth. Unveiling N mineralization (Nm) process characteristics and developing a simple and effective approach to evaluate soil Nm are imperative to guide N fertilizer application and enhance its efficiency in various paddy soils with different physicochemical properties. Soil properties are important driving factors contributing to soil Nm differences and must be considered to achieve effective N management. Nevertheless, discrepancies in Nm capacity and other key influencing factors remain uncertain. To address this knowledge gap, this study collected 52 paddy soil samples from Taihu Lake Basin, China, which possess vastly different physicochemical properties. The samples were subjected to a 112-d submerged anaerobic incubation experiment at a constant temperature to obtain the soil Nm characteristics. Reaction kinetics models, including one-pool exponential model, two-pool exponential model, and effective cumulative temperature model, were employed to compare characteristic differences between Nm potential (Nmp) and short-term accumulated mineralized N (Amn) processes in relation to soil physicochemical properties. Based on these relationships, simplified Nmp prediction methods for paddy soils were established. The results revealed that the Nmp values were 145.18, 88.64, and 21.03 mg kg-1 in paddy soils with pH < 6.50, 6.50 ≤ pH ≤ 7.50, and pH > 7.50, respectively. Significantly, short-term Amn at day 14 showed a good correlation (P < 0.01) with Nmp (R2 = 0.94), indicating that the prevailing short-term incubation experiment is an acceptable marker for Nmp. Moreover, Nmp correlated well with the ultraviolet absorbance value at 260 nm based on NaHCO3 extraction (Na260), further streamlining the Nmp estimation method. The incorporation of easily obtainable soil properties, including pH, total N (TN), and the ratio of total organic carbon to TN (C/N), alongside Na260 for Nmp evaluation allowed the multiple regression model, Nmp = 58.62 × TN - 23.18 × pH + 13.08 × C/N + 86.96 × Na260, to achieve a high prediction accuracy (R2 = 0.95). The reliability of this prediction was further validated with published data of paddy soils in the same region and other rice regions, demonstrating the regional applicability and prospects of this model. This study underscored the roles of soil properties in Nm characteristics and mechanisms and established a site-specific prediction model based on rapid extractions and edaphic properties of paddy soils, paving the way for developing rapid and precise Nm prediction models.
土壤矿化氮(N)是土壤供氮能力的重要组成部分,是水稻生长的重要氮源。揭示土壤氮素矿化过程特征,建立简单有效的土壤氮素矿化评价方法,是指导不同理化性质水稻土氮肥施用和提高氮肥效率的必要手段。土壤性质是影响土壤氮素差异的重要驱动因素,是实现有效氮素管理必须考虑的因素。然而,纳米容量的差异和其他关键影响因素仍然不确定。为了解决这一知识空白,本研究从中国太湖流域收集了52个水稻土样品,这些样品具有截然不同的物理化学性质。对样品进行112 d的恒温水下厌氧培养实验,获得土壤纳米特性。采用单池指数模型、双池指数模型和有效积温模型等反应动力学模型,比较纳米势(Nmp)和短期累积矿化氮(Amn)过程对土壤理化性质的特征差异。基于这些关系,建立了水稻土Nmp的简化预测方法。结果表明,在pH <; 6.50、6.50≤pH≤7.50和pH >; 7.50条件下,水稻土的Nmp值分别为145.18、88.64和21.03 mg kg-1。值得注意的是,第14天的短期Amn与Nmp呈良好的相关性(P < 0.01) (R2 = 0.94),表明目前流行的短期孵育实验是一个可接受的Nmp指标。此外,Nmp与NaHCO3提取(Na260)的260 nm紫外吸光度值具有良好的相关性,进一步简化了Nmp估算方法。将土壤pH、全氮(TN)、总有机碳与TN之比(C/N)等易于获取的土壤性质与Na260结合进行Nmp评价,使Nmp = 58.62 × TN - 23.18 × pH + 13.08 × C/N + 86.96 × Na260的多元回归模型具有较高的预测精度(R2 = 0.95)。利用已发表的同一地区和其他水稻区水稻土数据进一步验证了该预测的可靠性,证明了该模型的区域适用性和应用前景。本研究强调了土壤性质在纳米粒特征中的作用及其机制,并建立了基于水稻土快速提取和土壤性质的特定位点纳米粒预测模型,为建立快速、精确的纳米粒预测模型奠定了基础。
{"title":"Efficiency-enhancing methods for predicting nitrogen mineralization characteristics in paddy soils using soil properties and rapid soil extractions","authors":"Yujuan LIU ,&nbsp;Yuqi CHEN ,&nbsp;Xiuyun LIU ,&nbsp;Siyuan CAI ,&nbsp;Jiahui YUAN ,&nbsp;Lingying XU ,&nbsp;Yu WANG ,&nbsp;Xu ZHAO ,&nbsp;Xiaoyuan YAN","doi":"10.1016/j.pedsph.2024.10.001","DOIUrl":"10.1016/j.pedsph.2024.10.001","url":null,"abstract":"<div><div>Soil mineralized nitrogen (N) is a vital component of soil N supply capacity and an important N source for rice growth. Unveiling N mineralization (Nm) process characteristics and developing a simple and effective approach to evaluate soil Nm are imperative to guide N fertilizer application and enhance its efficiency in various paddy soils with different physicochemical properties. Soil properties are important driving factors contributing to soil Nm differences and must be considered to achieve effective N management. Nevertheless, discrepancies in Nm capacity and other key influencing factors remain uncertain. To address this knowledge gap, this study collected 52 paddy soil samples from Taihu Lake Basin, China, which possess vastly different physicochemical properties. The samples were subjected to a 112-d submerged anaerobic incubation experiment at a constant temperature to obtain the soil Nm characteristics. Reaction kinetics models, including one-pool exponential model, two-pool exponential model, and effective cumulative temperature model, were employed to compare characteristic differences between Nm potential (Nmp) and short-term accumulated mineralized N (Amn) processes in relation to soil physicochemical properties. Based on these relationships, simplified Nmp prediction methods for paddy soils were established. The results revealed that the Nmp values were 145.18, 88.64, and 21.03 mg kg<sup>-1</sup> in paddy soils with pH &lt; 6.50, 6.50 ≤ pH ≤ 7.50, and pH &gt; 7.50, respectively. Significantly, short-term Amn at day 14 showed a good correlation (<em>P</em> &lt; 0.01) with Nmp (<em>R</em><sup>2</sup> = 0.94), indicating that the prevailing short-term incubation experiment is an acceptable marker for Nmp. Moreover, Nmp correlated well with the ultraviolet absorbance value at 260 nm based on NaHCO<sub>3</sub> extraction (Na260), further streamlining the Nmp estimation method. The incorporation of easily obtainable soil properties, including pH, total N (TN), and the ratio of total organic carbon to TN (C/N), alongside Na260 for Nmp evaluation allowed the multiple regression model, Nmp = 58.62 × TN - 23.18 × pH + 13.08 × C/N + 86.96 × Na260, to achieve a high prediction accuracy (<em>R</em><sup>2</sup> = 0.95). The reliability of this prediction was further validated with published data of paddy soils in the same region and other rice regions, demonstrating the regional applicability and prospects of this model. This study underscored the roles of soil properties in Nm characteristics and mechanisms and established a site-specific prediction model based on rapid extractions and edaphic properties of paddy soils, paving the way for developing rapid and precise Nm prediction models.</div></div>","PeriodicalId":49709,"journal":{"name":"Pedosphere","volume":"35 6","pages":"Pages 1054-1064"},"PeriodicalIF":7.3,"publicationDate":"2024-10-04","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"145555059","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":2,"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
Nano-sized humic acid improves phosphate fertiliser efficiency in chilli pepper 纳米腐植酸提高了辣椒磷肥利用率
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-09-24 DOI: 10.1016/j.pedsph.2024.09.007
Qizhong XIONG , Shaojie WANG , Xuxiang CHEN , Jianyuan JING , Yonglin JIN , Hongying LI , Chaochun ZHANG , Yuji JIANG , Xinxin YE
Humic acid (HA) prevents phosphorus (P) fixation and promotes P absorption by plants, thereby effectively increasing the efficiency of phosphate fertiliser utilisation. Although nano-sized HA (NHA) might exhibit superior effects compared to conventional-sized HA (CHA), evidence is limited. Therefore, we investigated the effects of CHA and NHA applied with conventional phosphate fertiliser (CHA+CP and NHA+CP, respectively) on chilli pepper biomass, P uptake, and root morphology, as well as soil available P content, and evaluated CHA, NHA, and their residues in the soil for differences in specific surface area, functional groups, molecular weight distribution, and surface elemental compositions in a 40-d pot cultivation experiment. Results showed that the CHA+CP and NHA+CP treatments significantly increased pepper biomass and P uptake by 15.2%–24.7% and 37.9%–49.0%, respectively, compared to the conventional phosphate fertiliser applied alone (CP) treatment (P < 0.05), with NHA exhibiting a greater effect than CHA. This was primarily related to NHA's stronger ability to reduce P fixation than that of CHA. Soil available P content significantly increased by 5.8% and 3.8% in the NHA+CP treatment compared with CHA+CP on days 22 and 40 of cultivation, respectively (P < 0.05). Nano-sized HA contained more small-molecule components and carboxyl groups than CHA, which can more stimulate root elongation and thus promote root P uptake. Furthermore, fertiliser-derived P gradually entered the structure of CHA or NHA during cultivation. The presence of more plant-available forms (e.g., H2 PO4 and HPO42-) in NHA compared to CHA also contributed to better regulation of phosphate fertiliser efficacy. In conclusion, NHA is superior to CHA in improving phosphate fertiliser efficiency, making it a potential alternative material for the development of high-efficiency phosphate fertilisers. This presents an excellent opportunity to minimise P resource waste.
腐植酸(HA)阻止磷(P)的固定,促进植物对磷的吸收,从而有效提高磷肥的利用效率。尽管纳米级透明质酸(NHA)可能比常规级透明质酸(CHA)表现出更好的效果,但证据有限。因此,本研究在常规磷肥(分别为CHA+CP和NHA+CP)下施用CHA和NHA对辣椒生物量、磷吸收量、根系形态和土壤速效磷含量的影响,并通过40 d盆栽试验评价CHA、NHA及其在土壤中的残留量在比表面积、官能团、分子量分布和表面元素组成方面的差异。结果表明:CHA+CP和NHA+CP处理较常规单施磷肥(CP)处理显著提高了辣椒生物量和磷吸收量,分别提高了15.2% ~ 24.7%和37.9% ~ 49.0% (P < 0.05),其中NHA的作用大于CHA。这主要与NHA比CHA具有更强的降低固磷能力有关。栽培第22天和第40天,NHA+CP处理土壤速效磷含量较CHA+CP分别显著提高5.8%和3.8% (P < 0.05)。纳米HA比CHA含有更多的小分子成分和羧基,能更好地刺激根系伸长,从而促进根系对磷的吸收。此外,在栽培过程中,肥料衍生的磷逐渐进入CHA或NHA结构。与CHA相比,NHA中存在更多的植物可利用形态(例如H2PO4−和HPO42-),也有助于更好地调节磷肥功效。综上所述,NHA在提高磷肥效率方面优于CHA,是开发高效磷肥的潜在替代材料。这提供了一个极好的机会,以尽量减少磷资源浪费。
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引用次数: 0
Numerical analysis of thermo-water-vapor-carbon coupling in a permafrost region: A case study in the Beiluhe region of the Qingzang Plateau, China 多年冻土区热-水-汽-碳耦合的数值分析——以青藏高原北麓河地区为例
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-09-24 DOI: 10.1016/j.pedsph.2024.09.006
Haotian WEI , Enlong LIU , Chuan HE , Bingtang SONG , Dan WANG , Jian KANG , Ling CHEN , Qiong LI
With global warming and the intensification of human activities, frozen soils continue to melt, leading to the formation of thermokarst collapses and thermokarst lakes. The thawing of permafrost results in the microbial decomposition of large amounts of frozen organic carbon (C), releasing greenhouse gases such as carbon dioxide (CO2) and methane (CH4). However, little research has been done on the thermo-water-vapor-carbon coupling process in permafrost, and the interactions among hydrothermal transport, organic matter decomposition, and CO2 transport processes in permafrost remain unclear. We considered the decomposition and release of organic C and established a coupled thermo-water-vapor-carbon model for permafrost based on the study area located in the Beiluhe region of the Qingzang Plateau, China. The model established accurately reflected changes in permafrost temperature, moisture, and C fluxes. Dramatic changes in temperature and precipitation in the warm season led to significant soil water and heat transport, CO2 transport, and organic matter decomposition. During the cold season, however, the soil froze, which weakened organic matter decomposition and CO2 transport. The sensitivity of soil layers to changes in the external environment varied with depth. Fluctuations in energy, water, and CO2 fluxes were greater in shallow soil layers than in deeper ones. The latent heat of water-vapor and water-ice phase changes played a crucial role in regulating the temperature of frozen soil. The low content of soil organic matter in the study area resulted in a smaller influence of the decomposition heat of soil organic matter on soil temperature, compared to the high organic matter content in other soil types (such as peatlands).
随着全球变暖和人类活动的加剧,冻土不断融化,形成热岩溶塌陷和热岩溶湖。永久冻土的解冻导致微生物分解大量冻结的有机碳(C),释放出二氧化碳(CO2)和甲烷(CH4)等温室气体。然而,对多年冻土中热-水-汽-碳耦合过程的研究较少,热液运移、有机质分解和CO2运移过程之间的相互作用尚不清楚。考虑有机碳的分解和释放,以青藏高原北麓河地区为研究区,建立了多年冻土热-水-汽-碳耦合模型。所建立的模型准确地反映了永久冻土温度、水分和碳通量的变化。暖季气温和降水的剧烈变化导致土壤水热输运、CO2输运和有机质分解显著。然而,在寒冷季节,土壤冻结,这削弱了有机物的分解和二氧化碳的运输。土层对外部环境变化的敏感性随土层深度的不同而不同。能量、水和二氧化碳通量的波动在浅层土壤中比在深层土壤中更大。水汽潜热和水冰相变对冻土温度的调节起着重要作用。研究区土壤有机质含量较低,土壤有机质分解热对土壤温度的影响较小,而其他土壤类型(如泥炭地)有机质含量较高。
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引用次数: 0
Impacts of microplastics, fluoride and mancozeb on tomato plant growth and rhizosphere microbial dynamics: A metagenomic analysis 微塑料、氟化物和代森锰锌对番茄植株生长和根际微生物动力学的影响:宏基因组分析
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-09-17 DOI: 10.1016/j.pedsph.2024.09.001
Ajay KUMAR , Rajni SHARMA , Muskan BOKOLIA , Riyapi DAS , Sanjiv KUMAR , Ravindresh CHABBRA , Baljinder SINGH
Microplastics (MPs), fluoride (FR), and fungicide mancozeb (MZ) are common contaminants in soil. However, there is no information about the combined impacts of MPs, FR, and MZ on tomato plant growth features in the literature. This study aimed to investigate the effects of combined application of MPs, FR, and MZ (both analytical grade and commercial) on the growth and development of tomato plants and metagenomics of rhizosphere soil. A pot experiment was set up in an artificial greenhouse with two sets of treatments. One set was the combined application of MPs, FR, and analytical grade MZ (B2) and a control without the application of MPs, FR, and MZ (W2), and the other set was the combined application of MPs, FR, and commercial MZ (B3) and a control without the application of MPs, FR, and MZ (W3). No detrimental effects of MPs, FR, and MZ were detected on the growth parameters of tomato plants, including the number of leaves and chlorophyll concentration. However, tomato roots showed knot and nodulation-type structures, and metabolomic profiling revealed that combined exposure to MPs, FR, and MZ profoundly reprogrammed the primary metabolism in tomato roots, with marked alterations in carbohydrate and amino acid pathways. Metagenome whole genome sequencing showed that the B2 and B3 treatments profoundly affected soil microbial community composition, diversity, gene abundances, and functional gene variations compared to W2 and W3. Proteobacteria became the dominating phylum in B2 and B3, causing a significant shift in the microbiome. Its abundance soared to 66.7% in B2 and 75.4% in B3, compared to only 35.9% in W2 and 28.9% in W3. On the other hand, Actinobacteria decreased significantly from 55.6% in W2 and 63.8% in W3 to 18.1% in B2 and 9.6% in B3. This study highlights the microbial shifts due to combined application of MPs, FR, and MZ, providing evidence for understanding their environmental risks.
微塑料(MPs)、氟化物(FR)和杀菌剂代森锰锌(MZ)是土壤中常见的污染物。然而,文献中尚未见MPs、FR和MZ对番茄植株生长特性的联合影响。本研究旨在研究分析级和市售级多磺酸钠(MPs)、多磺酸钠(FR)和多磺酸钠(MZ)配施对番茄植株生长发育和根际土壤宏基因组学的影响。在人工温室进行盆栽试验,采用两套处理方法。一组是MPs、FR和分析级MZ (B2)的联合应用,另一组是MPs、FR和MZ的联合应用(W2),另一组是MPs、FR和商业MZ (B3)的联合应用,另一组是MPs、FR和MZ的联合应用(W3)。MPs、FR和MZ对番茄植株叶片数和叶绿素浓度等生长参数均无不良影响。然而,番茄根系显示出结瘤型结构,代谢组学分析显示,MPs、FR和MZ的联合暴露深刻地重新编程了番茄根系的初级代谢,碳水化合物和氨基酸途径发生了显著变化。宏基因组全基因组测序结果表明,与W2和W3相比,B2和B3处理对土壤微生物群落组成、多样性、基因丰度和功能基因变异均有显著影响。变形菌门成为B2和B3的主导门,引起微生物组的显著变化。B2和B3的丰度分别为66.7%和75.4%,而W2和W3的丰度分别为35.9%和28.9%。放线菌数量从W2的55.6%和W3的63.8%显著下降到B2的18.1%和B3的9.6%。本研究强调了MPs、FR和MZ联合应用导致的微生物变化,为理解它们的环境风险提供了证据。
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引用次数: 0
Effects of rice cropping method and growth stage on rhizosphere bacterial diversity and soil biological attributes 水稻种植方式和生育期对根际细菌多样性和土壤生物学特性的影响
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-09-07 DOI: 10.1016/j.pedsph.2024.08.010
Surathi ADITHYA, Sai Aparna Devi NUNNA, Chinnappan CHINNADURAI, Dananjeyan BALACHANDAR
Rice cropping method is primarily decided by soil moisture regime. System of rice intensification (SRI) and direct-seeded aerobic rice are two primary modifications of traditional wetland rice. Understanding rice rhizosphere microbiome and functioning as influenced by these cropping methods is essential for sustaining rice productivity. The objective of this study was to assess the impact of three different rice cropping methods (wetland rice, SRI, and aerobic rice) on the biochemical properties and bacterial communities within the rice rhizosphere across three key rice growth stages: tillering, flowering, and maturity. Soil organic carbon (SOC), microbial biomass carbon (MBC), dehydrogenase activity, substrate-induced respiration (SIR), and metabolic quotient (MQ) were assessed along with high-throughput 16S rRNA sequencing of rice rhizosphere soils. The rice rhizosphere soil registered the highest SOC, MBC, and dehydrogenase activity in SRI followed by wetland rice and then aerobic rice. Cropping method had a minimal impact on SIR and MQ. Along with cropping method, growth stage also significantly altered these biological attributes of rice rhizosphere. The trends of the highest SOC content and dehydrogenase activity at the flowering stage and the highest MBC content and SIR at the tillering stage of rice were observed in all three rice cropping methods. The analysis of bacterial communities, based on 16S rRNA gene sequencing, revealed that both cropping method and growth stage significantly impacted the composition of rhizosphere microbiomes. However, the influence of cropping method was less pronounced compared to growth stage. Cropping method caused notable shifts in the abundances of Proteobacteria, Bacteroidetes, and Chloroflexi, while growth stage affected the abundances of Proteobacteria, Actinobacteria, Cyanobacteria, Firmicutes, Chloroflexi, and Bacteroidetes. Based on these results, the SRI method led to higher diversification to the rhizosphere bacteriobiota, as well as greater incorporation of carbon into the soil and increased dehydrogenase activity compared to wetland rice and aerobic rice. This study deepens our understanding of how different cropping methods influence plant-microbe interaction and the implications for overall rice productivity and soil health.
水稻的种植方式主要取决于土壤水分状况。水稻集约化系统和旱作水稻是传统湿地水稻的两种主要改良方式。了解这些种植方式对水稻根际微生物群及其功能的影响对维持水稻生产力至关重要。本研究的目的是评估三种不同的水稻种植方式(湿地稻、SRI稻和好氧稻)对水稻分蘖期、开花期和成熟期三个关键生育期水稻根际生化特性和细菌群落的影响。采用高通量16S rRNA测序技术对水稻根际土壤有机碳(SOC)、微生物生物量碳(MBC)、脱氢酶活性、底物诱导呼吸(SIR)和代谢商(MQ)进行了测定。水稻根际土壤有机碳、MBC和脱氢酶活性最高,湿地稻次之,好氧稻次之。裁剪方法对SIR和MQ的影响最小。随着种植方式的不同,生育期也显著改变了水稻根际的这些生物学特性。3种水稻种植方式的有机碳含量和脱氢酶活性在开花期最高,MBC含量和SIR在分蘖期最高。基于16S rRNA基因测序的细菌群落分析显示,种植方式和生育期对根际微生物群落组成有显著影响。但不同种植方式对生育期的影响不明显。种植方式对变形菌门、拟杆菌门和拟绿杆菌门的丰度有显著影响,而生长阶段对变形菌门、放线菌门、蓝藻门、厚壁菌门、拟绿杆菌门的丰度有显著影响。基于这些结果,与湿地水稻和有氧水稻相比,SRI方法使根际菌群多样化程度更高,土壤中的碳含量更高,脱氢酶活性也更高。这项研究加深了我们对不同种植方式如何影响植物-微生物相互作用以及对水稻整体生产力和土壤健康的影响的理解。
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引用次数: 0
Complementing culture-dependent and -independent approaches is essential when assessing bacterial community potential functions in chronically polycyclic aromatic hydrocarbon-contaminated soils 在评估慢性多环芳烃污染土壤中细菌群落的潜在功能时,补充培养依赖和独立的方法是必不可少的
IF 7.3 2区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-09-07 DOI: 10.1016/j.pedsph.2024.08.005
Sabrina FESTA , Esteban Emanuel NIETO , Penélope RAPOSEIRAS ALDORINO , Sara CUADROS-ORELLANA , José Matías IRAZOQUI , Claudio QUEVEDO , Bibiana Marina COPPOTELLI , Irma Susana MORELLI
Bioremediation is an eco-friendly alternative for soil restoration. However, its outcomes are still variable. Different bioremediation strategies were used in a chronically polycyclic aromatic hydrocarbon (PAH)-contaminated soil, and no degradation was achieved. This work attempts to study whether the soil bacterial community has the genetic potential for aromatic compound degradation (ACD). While 16S rRNA metabarcoding of that soil showed a predominance of Proteobacteria, shotgun metagenomics indicated that 99.5% of the sequences were taxonomically assigned to Streptomycetales, and almost all genes related to ACD were assigned to the latter. As comprehension of the composition and metabolic potential of a soil community can be enhanced by exploring enrichment cultures of that soil, a culture approach followed by a shotgun metagenomic analysis was performed. These enrichment cultures were obtained by sequential transfers with pyrene conducted every 7 (r-EFP) and 28 (k-MSP2) d. Both r-EFP and k-MSP2 demonstrated the ability to degrade pyrene and the presence of genes related to ACD. While Pseudomonas and Olivibacter were the predominant genera in r-EFP, Mycobacterium, Chitoniphaga, Bacillus, and Pseudoxanthomonas were predominant in k-MSP2. This study demonstrated the soil bacterial community's potential to degrade PAHs of three and four rings. Therefore, exploration of bioremediation strategies aimed at activating this potential would be worthwhile. It was confirmed that shotgun metagenomics may not fully reveal potential bacterial functions when characterizing impacted soil microbiomes. Additionally, culture-based methods complemented and increased the knowledge obtained from culture-independent approaches, demonstrating their utility for bioprospecting PAH degraders and designing microbiome engineering strategies.
生物修复是一种生态友好的土壤修复方法。然而,其结果仍然是多变的。对慢性多环芳烃(PAH)污染土壤采用不同的生物修复策略,均未达到降解效果。本文旨在研究土壤细菌群落是否具有降解芳香族化合物的遗传潜力。土壤16S rRNA元条形码显示Proteobacteria占优势,shotgun元基因组分析显示99.5%的序列属于Streptomycetales,几乎所有与ACD相关的基因都属于后者。由于可以通过探索土壤的富集培养来增强对土壤群落组成和代谢潜力的理解,因此采用了一种培养方法,然后进行了霰弹枪宏基因组分析。这些富集培养物是通过每7天(r-EFP)和28天(k-MSP2)进行芘的连续转移获得的。r-EFP和k-MSP2都显示出降解芘的能力,并且存在与ACD相关的基因。r-EFP以假单胞菌属和橄榄杆菌属为主,k-MSP2以分枝杆菌属、壳噬菌体属、芽孢杆菌属和假黄单胞菌属为主。本研究证明了土壤细菌群落对三环和四环多环芳烃的降解潜力。因此,探索旨在激活这种潜力的生物修复策略是值得的。在表征受影响的土壤微生物组时,霰弹枪宏基因组学可能无法完全揭示潜在的细菌功能。此外,基于培养的方法补充并增加了从非培养方法中获得的知识,证明了它们在生物勘探多环芳烃降解物和设计微生物组工程策略方面的实用性。
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引用次数: 0
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Pedosphere
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