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Vegetation restoration changed the soil aggregate stability and aggregate carbon stabilization pathway according to δ13C signatures 根据 δ13C 信号,植被恢复改变了土壤团聚稳定性和团聚碳稳定途径
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-10-03 DOI: 10.1016/j.agee.2024.109317
Zhuoxia Su , Shu Zhu , Zhenhao Wei , Yanxing He , Bingqian Su , Kang Zhang , Xing Ma , Zhouping Shangguan
Vegetation restoration can increase soil organic carbon (SOC) sequestration through the physical protection of soil aggregates. However, the soil aggregate stability and C flow pathway associated with long-term plantation restoration have not yet been fully characterized. Here, we conducted a study on Robinia pseudoacacia plantations at different recovery stages, studied the distribution and stability of aggregates, analysed the aggregate-associated organic carbon (OC) content and δ13C value, and quantified the aggregate C flow pathway. The results revealed that vegetation restoration increased the proportion of large macroaggregates (LMAs) and decreased the proportion of small macroaggregates (SMAs), with no changes observed in the proportion of microaggregates (MIAs) or silt + clay (SC) at 0–20 cm. The indices of aggregate stability, namely, the mean weight diameter (MWD), geometric mean diameter (GMD) and structural stability index (SSI), increased under vegetation restoration at 0–20 cm, with maximum values of 3.83 mm, 2.88 mm, and 2.00 %, respectively, at 35 years of age (35Y). The OC content of the LMAs increased from 10.96 to 21.64 g kg−1 and from 7.27 to 10.05 g kg−1 in the 0–20 cm and 20–40 cm layers, respectively. LMAs and SMAs had the greatest contributions to SOC accumulation in the 0–20 cm and 20–40 cm layers, respectively. The δ13C value increased with decreasing aggregate size. The C flow pathway was from macroaggregates to MIAs or SC. Compared with abandoned farmland, vegetation restoration decreased the aggregate C flow intensity in the 0–20 cm layer. The soil aggregate stability and aggregate-associated OC content decreased with increasing soil depth, but the soil δ13C value exhibited the opposite trend. Vegetation restoration regulated soil aggregate stability by influencing the fine root biomass (FRB) and SOC content. In summary, our analysis offers a valuable reference for the controlling effect of aggregation on C stability influenced by vegetation restoration.
植被恢复可以通过对土壤团聚体的物理保护增加土壤有机碳(SOC)的固存。然而,与长期植被恢复相关的土壤团聚体稳定性和碳流动途径尚未得到充分表征。在此,我们对不同恢复阶段的刺槐人工林进行了研究,研究了聚合体的分布和稳定性,分析了与聚合体相关的有机碳(OC)含量和δ13C 值,并量化了聚合体碳流路径。结果表明,植被恢复增加了大型聚集体(LMAs)的比例,降低了小型聚集体(SMAs)的比例,0-20 厘米处的微聚集体(MIAs)和粉土+粘土(SC)的比例没有变化。骨料稳定性指数,即平均重量直径(MWD)、几何平均直径(GMD)和结构稳定性指数(SSI)在 0-20 厘米植被恢复条件下有所增加,35 年龄期(35Y)时的最大值分别为 3.83 毫米、2.88 毫米和 2.00%。在 0-20 厘米层和 20-40 厘米层,LMA 的 OC 含量分别从 10.96 克/千克增至 21.64 克/千克,从 7.27 克/千克增至 10.05 克/千克。LMA 和 SMA 分别对 0-20 厘米和 20-40 厘米层的 SOC 积累贡献最大。δ13C值随着骨料粒径的减小而增加。C的流动途径是从大集料到MIAs或SC。与废弃农田相比,植被恢复降低了 0-20 cm 土层的集料碳流强度。土壤团聚体稳定性和团聚体相关 OC 含量随土壤深度的增加而降低,但土壤 δ13C 值却呈现出相反的趋势。植被恢复通过影响细根生物量(FRB)和 SOC 含量来调节土壤团聚体稳定性。总之,我们的分析为植被恢复对C稳定性的聚合控制作用提供了有价值的参考。
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引用次数: 0
Water-saving irrigation practices in rice paddies reverse the impact of root aerenchyma on methane emissions 水稻田节水灌溉措施可逆转根瘤对甲烷排放的影响
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-10-02 DOI: 10.1016/j.agee.2024.109309
Siyu Li , Yajun Zhang , Jiamei Zhao , Kees Jan van Groenigen , Xinya Shen , Hao Zhang , Junfei Gu , Weiyang Zhang , Dafeng Hui , Yun Chen , Lijun Liu
Rice root aerenchyma (RA) and irrigation practices influence key physiological processes in rice paddies, affecting both yield and methane (CH4) emissions. However, the interaction between RA and irrigation practices, and its implications for CH4 mitigation, remains unclear, making it difficult to identify rice cultivars for CH4 mitigation purposes. Here, we conducted a series of field and pot experiments to evaluate how RA affects grain yield and CH4 emissions under two common irrigation regimes: continuous flooding (CF) and alternate wetting and drying (AWD). Our results show that the interaction between RA and irrigation regime significantly influenced both rice yield and CH4 emissions. Under CF, increased RA formation was associated with higher rice yield and lower CH4 emissions across a wide range of cultivars. These results could be explained by cultivars with well-developed RA increasing root oxygen loss, thereby stimulating CH4 oxidation and promoting N availability to support plant growth. In AWD systems, no significant differences in rice yield, methanogenesis or methanotrophy were observed between cultivars with varying RA development. However, cultivars with well-developed RA increased CH4 emissions by 28 %−32 % compared to those with less-developed RA, likely due to enhanced CH4 transport from anaerobic deep soil layers to the atmosphere. Consistent with these findings, CH4 emissions under AWD decreased when we inhibited RA development through root irrigation with brassinosteroids. In conclusion, we demonstrate that AWD in paddies can reverse the impact of RA on CH4 emissions, highlighting the need for CH4 mitigation strategies involving cultivar selection to account for variations in irrigation practices.
水稻根部气孔(RA)和灌溉方法会影响稻田的关键生理过程,从而影响产量和甲烷(CH4)排放。然而,RA 与灌溉方式之间的相互作用及其对甲烷减排的影响仍不清楚,因此很难确定用于甲烷减排的水稻品种。在此,我们进行了一系列田间和盆栽实验,以评估在两种常见灌溉制度(连续淹水(CF)和干湿交替(AWD))下 RA 如何影响谷物产量和 CH4 排放。结果表明,RA 与灌溉制度之间的相互作用对水稻产量和甲烷排放量都有显著影响。在 CF 条件下,RA 形成的增加与水稻产量的提高和各种栽培品种的 CH4 排放量的降低有关。这些结果可能是由于RA发达的栽培品种增加了根部的氧气损失,从而刺激了CH4氧化,促进了氮的供应以支持植物生长。在 AWD 系统中,RA 不同的栽培品种在水稻产量、甲烷生成或甲烷营养方面没有明显差异。然而,与RA发育程度较低的品种相比,RA发育良好的品种CH4排放量增加了28%-32%,这可能是由于CH4从厌氧深层土壤向大气传输的能力增强所致。与这些发现一致的是,当我们通过使用黄铜类固醇灌根来抑制 RA 的发育时,AWD 条件下的 CH4 排放量会减少。总之,我们证明了水稻全灌溉可以逆转RA对CH4排放的影响,这突出表明需要制定CH4减缓策略,包括选择栽培品种,以考虑灌溉方法的变化。
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引用次数: 0
Evidence at the landscape level links high predator/pest ratios to biocontrol services against aphids 景观层面的证据将捕食者/害虫的高比例与针对蚜虫的生物控制服务联系起来
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-10-02 DOI: 10.1016/j.agee.2024.109319
Bing Liu , Yanhui Lu
Compared with external environment interferences, the interaction between arthropod natural enemies and pests is the key inherent driver determining the strength of biocontrol services. However, the extent to which this effect can suppress pests is still inconclusive. We combined two complementary experiments to determine how variation in an assemblage of generalist arthropod predators modified the level of biocontrol services for suppression of a key aphid pest in cotton fields. Using generalized linear mixed effect models (GLMM) and path analysis, we clarified the causal relationship between predator/aphid ratios (PAR) and (1) the resulting biocontrol services index (BSI) and (2) the aphid population growth index (APGI) as seen in field predator exclusion trials. We also measured the effect of PAR on APGI in more commercial cotton fields. Our results, at landscape level, indicate that when PAR values increased one unit, BSI values improved 34.1 %, and reduced aphid population growth 28.3 % (the standardized effect coefficient in path analysis) during two weeks in field cage-exclusion trials. The effect of high predator/aphid ratios on reducing the aphid population growth rates was also significant in more commercial cotton fields, which were sampled over a longer time interval (4 weeks). Our study confirmed that there was a causal relationship between the natural enemy/pest ratio and the level of biological pest control services for predators and aphid population growth in crop fields. PAR values (predator/aphid ratios) can, therefore, be used to predict the level of biocontrol services in this context instead of relying on more labor-intensive cage exclusion studies.
与外部环境干扰相比,节肢动物天敌与害虫之间的相互作用是决定生物防治服务强度的关键内在驱动因素。然而,这种作用能在多大程度上抑制害虫仍无定论。我们结合了两个互补实验,以确定广义节肢动物捕食者集合体的变化如何改变生物防治服务的水平,从而抑制棉田中的一种主要蚜虫害虫。利用广义线性混合效应模型(GLMM)和路径分析,我们明确了捕食者/蚜虫比率(PAR)与(1)由此产生的生物防治服务指数(BSI)和(2)蚜虫种群增长指数(APGI)之间的因果关系。我们还在更多的商业棉田中测量了 PAR 对 APGI 的影响。我们在景观层面的结果表明,当 PAR 值增加一个单位时,BSI 值提高了 34.1%,在两周的田间笼养驱避试验中,蚜虫数量增长减少了 28.3%(路径分析中的标准化效应系数)。高捕食者/蚜虫比对降低蚜虫种群增长率的影响在采样时间间隔更长(4 周)的更多商业棉田中也很显著。我们的研究证实,天敌/害虫比和天敌生物防治害虫服务水平与作物田中的蚜虫数量增长之间存在因果关系。因此,PAR 值(捕食者/蚜虫比率)可用于预测生物防治服务的水平,而不是依赖劳动密集型笼舍排除研究。
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引用次数: 0
Cropland-scale interaction between maize evapotranspiration and groundwater in a well-irrigation district in Mu Us Sandy Land, Northwest China 中国西北部木乌斯沙地井灌区玉米蒸散量与地下水之间的耕地尺度相互作用
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-10-01 DOI: 10.1016/j.agee.2024.109282
Lizhu Hou , Xu-Sheng Wang , Yangxiao Zhou , Guibing Zhu , Yuesheng Gao , Jiangyi Zhou
The knowledge of the water fluxes and groundwater contributions to plant water use under fluctuating groundwater levels is crucial for the sustainable utilization of groundwater resources and the preservation of healthy ecosystems in semi-arid regions, such as the desert oasis croplands in the Mu Us Sandy Land (MUSL), Northwest China. A 3-year field trial was conducted in an oasis cropland within MUSL, involving five treatments with surface irrigation depths ranging from 5 mm to 60 mm per application and 5 to 11 irrigation applications per year. The major physical characteristics of the soils at the site were ascertained through laboratory measurements. Hydrogen and oxygen isotopes (deuterium and oxygen 18) in different water sources for the treatment with an irrigation depth of 45 mm per application (I45) in the maize field were analyzed from in situ samples, and root water uptake (RWU) was further identified using the IsoSource model. A numerical model based on HYDRUS-1D for soil water fluxes was calibrated and validated using observation data to estimate the actual evapotranspiration (ETa) and water productivity (WP) under various irrigation treatments. The isotope analysis indicated that maize water uptake in the I45 treatment incorporated both groundwater and soil water during the growing stage. The large negative d-excess values in groundwater suggested a secondary evaporation effect of recharge water due to irrigation return flow. According to simulations with Hydrus-1D, groundwater use contributed 9 % to 37 % of the maize ETa for the I45 treatment between 2014 and 2016 when the depth to the water table varied between 0.81 m and 1.13 m. With an optimal irrigation depth of 37 mm per application, the maximum yield and WP can be achieved in oasis cropland. Even in dry years, with a 16 % probability of rainfall occurrence, maize production was not affected due to the capillary rise of groundwater and the pumping of groundwater for irrigation. These results offer potential scientific insights for agricultural water management of spring maize under irrigation in desert oasis farmlands of the MUSL and other regions with similar soil texture, climatic conditions, and cropping practices.
了解地下水位波动下的水通量和地下水对植物用水的贡献对于半干旱地区地下水资源的可持续利用和保护健康的生态系统至关重要,例如中国西北部的木乌苏沙地(MUSL)荒漠绿洲耕地。在木乌苏沙地的绿洲耕地上进行了为期 3 年的田间试验,共设 5 个处理,地表灌溉深度从 5 毫米到 60 毫米不等,每年灌溉 5 到 11 次。通过实验室测量确定了该地点土壤的主要物理特征。对玉米田中每次灌溉深度为 45 毫米的处理(I45)的不同水源中的氢和氧同位素(氘和氧 18)进行了现场取样分析,并利用 IsoSource 模型进一步确定了根系吸水量(RWU)。利用观测数据对基于 HYDRUS-1D 的土壤水通量数值模型进行了校准和验证,以估算各种灌溉处理下的实际蒸散量(ETa)和水分生产率(WP)。同位素分析表明,在 I45 处理中,玉米在生长阶段吸收了地下水和土壤水。地下水中较大的负 d-excess 值表明,灌溉回流造成了补给水的二次蒸发效应。根据 Hydrus-1D 的模拟结果,2014 年至 2016 年期间,当地下水位深度在 0.81 米至 1.13 米之间时,地下水的使用占 I45 处理玉米蒸散发的 9%至 37%。绿洲耕地的最佳灌溉深度为 37 毫米/次,可实现最高产量和可湿性粉剂。即使在降雨概率为 16% 的干旱年份,玉米产量也不会因地下水毛细管上升和抽取地下水灌溉而受到影响。这些结果为在毛里求斯沙漠绿洲农田和其他具有类似土壤质地、气候条件和种植方式的地区灌溉春玉米的农业用水管理提供了潜在的科学启示。
{"title":"Cropland-scale interaction between maize evapotranspiration and groundwater in a well-irrigation district in Mu Us Sandy Land, Northwest China","authors":"Lizhu Hou ,&nbsp;Xu-Sheng Wang ,&nbsp;Yangxiao Zhou ,&nbsp;Guibing Zhu ,&nbsp;Yuesheng Gao ,&nbsp;Jiangyi Zhou","doi":"10.1016/j.agee.2024.109282","DOIUrl":"10.1016/j.agee.2024.109282","url":null,"abstract":"<div><div>The knowledge of the water fluxes and groundwater contributions to plant water use under fluctuating groundwater levels is crucial for the sustainable utilization of groundwater resources and the preservation of healthy ecosystems in semi-arid regions, such as the desert oasis croplands in the Mu Us Sandy Land (MUSL), Northwest China. A 3-year field trial was conducted in an oasis cropland within MUSL, involving five treatments with surface irrigation depths ranging from 5 mm to 60 mm per application and 5 to 11 irrigation applications per year. The major physical characteristics of the soils at the site were ascertained through laboratory measurements. Hydrogen and oxygen isotopes (deuterium and oxygen 18) in different water sources for the treatment with an irrigation depth of 45 mm per application (I<sub>45</sub>) in the maize field were analyzed from in situ samples, and root water uptake (<em>RWU</em>) was further identified using the IsoSource model. A numerical model based on HYDRUS-1D for soil water fluxes was calibrated and validated using observation data to estimate the actual evapotranspiration (<em>ET</em><sub>a</sub>) and water productivity (<em>WP</em>) under various irrigation treatments. The isotope analysis indicated that maize water uptake in the I<sub>45</sub> treatment incorporated both groundwater and soil water during the growing stage. The large negative d-excess values in groundwater suggested a secondary evaporation effect of recharge water due to irrigation return flow. According to simulations with Hydrus-1D, groundwater use contributed 9 % to 37 % of the maize <em>ET</em><sub>a</sub> for the I<sub>45</sub> treatment between 2014 and 2016 when the depth to the water table varied between 0.81 m and 1.13 m. With an optimal irrigation depth of 37 mm per application, the maximum yield and <em>WP</em> can be achieved in oasis cropland. Even in dry years, with a 16 % probability of rainfall occurrence, maize production was not affected due to the capillary rise of groundwater and the pumping of groundwater for irrigation. These results offer potential scientific insights for agricultural water management of spring maize under irrigation in desert oasis farmlands of the MUSL and other regions with similar soil texture, climatic conditions, and cropping practices.</div></div>","PeriodicalId":7512,"journal":{"name":"Agriculture, Ecosystems & Environment","volume":"378 ","pages":"Article 109282"},"PeriodicalIF":6.0,"publicationDate":"2024-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142417903","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
Divergent responses of soil aggregation and aggregate-carbon to fertilization regimes jointly explain soil organic carbon accrual in agroecosystems: A meta-analysis 土壤团聚和团聚碳对施肥制度的不同反应共同解释了农业生态系统中土壤有机碳的累积:荟萃分析
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-30 DOI: 10.1016/j.agee.2024.109314
Liwen Lin, Hao Chen, Yutao Peng, Junhui Yin, Junjie Guo, Chuntao He, Xiaochen Huang, Guorong Xin
Soil aggregation can be substantially affected by fertilizers and contributes to soil organic carbon (SOC) sequestration in agroecosystems. However, the mass and C distributions in different aggregates in responses to fertilization regimes are not often synchronous, which may largely affect soil C storage and stability. We conducted a meta-analysis of 2440 paired observations from 63 publications to assess the fertilization effects (i.e. inorganic, organic, and their combinations) on soil aggregation and aggregate-associated OC, as well as their linkages to the stimulated bulk soil C. Overall, fertilizer application significantly increased the mean weight diameter of soil aggregates by 27.8 %. The proportion of large (> 2 mm) and small (0.25–2 mm) macroaggregates were significantly increased by 19.8 % and 17.2 %, and that of microaggregate (0.053–0.25 mm) and silt-clay fraction (< 0.053 mm) were significantly decreased by 6.0 % and 18.4 %, respectively. In contrast, fertilization significantly increased C concentration in all aggregates. Organic fertilizer applications had remarkably greater effects than inorganic fertilizer applications on soil C concentration but the effects declined with decreasing aggregate size (from 36.5 % to 13.2 %), while that of inorganic application changed very little among aggregates (from 14.1 % to 10.0 %). The fertilizer effects on soil aggregation and aggregate-associated OC divergently responded to the gradients of major agronomic conditions (i.e. climate, soil properties, and duration). Organic fertilizer applications tended to have distinctly greater promotion effect than solely inorganic fertilizer applications with temperate climate, neutral-to-alkaline pH and more sand-like texture of soil. The importance of mineral- rather than larger size aggregate-associated OC in contributing to the bulk SOC pool tended to increase in the long term. The inorganic-organic combinations exhibited the most lasting effect on SOC accrual. In conclusion, the responses of bulk soil C to fertilizer applications were not always in accordance with those of soil aggregation, but can be well explained when jointly considering soil aggregate C. Our findings highlight the varying contributions of aggregates to the soil C pool in diverse and complicated agronomic situations, which are important to the agricultural C sink stability.
土壤团聚会受到肥料的很大影响,并有助于农业生态系统中土壤有机碳(SOC)的固存。然而,不同团聚体的质量和碳分布对施肥机制的响应往往并不同步,这可能会在很大程度上影响土壤碳的储存和稳定性。我们对 63 篇文献中的 2440 个配对观测数据进行了荟萃分析,以评估施肥(即无机肥、有机肥及其组合)对土壤团聚体和团聚体相关 OC 的影响,以及它们与受激发的土壤C总量之间的联系。大团聚体(> 2 mm)和小团聚体(0.25-2 mm)的比例分别显著增加了 19.8 % 和 17.2 %,微团聚体(0.053-0.25 mm)和粉土-粘土部分(< 0.053 mm)的比例分别显著减少了 6.0 % 和 18.4 %。与此相反,施肥则能明显提高所有集料中的碳浓度。施用有机肥对土壤碳浓度的影响明显大于施用无机肥,但随着团聚体大小的减小,有机肥的影响也在减小(从 36.5% 降至 13.2%),而施用无机肥对不同团聚体的影响变化很小(从 14.1% 降至 10.0%)。肥料对土壤团聚和团聚体相关有机碳的影响随主要农艺条件(即气候、土壤特性和持续时间)的变化而变化。在温带气候、pH 值为中性至碱性、土壤质地为沙土的条件下,施用有机肥的促进作用明显大于施用无机肥。从长远来看,矿物质而非更大粒径的聚合有机碳对大量有机碳库的贡献越来越大。无机-有机组合对 SOC 累积的影响最为持久。总之,大体积土壤碳对施肥的反应并不总是与土壤团聚体的反应一致,但如果共同考虑土壤团聚体碳,则可以很好地解释这一点。
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引用次数: 0
Grazing legacy mediates the diverse responses of grassland multidimensional stability to resource enrichment 放牧遗存介导草原多维稳定性对资源丰富性的不同反应
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-27 DOI: 10.1016/j.agee.2024.109313
Fengwei Xu , Jianjun Li , Liji Wu , Biao Zhu , Dima Chen , Yongfei Bai
Long-term grazing and resource enrichment are known to affect grassland ecosystem stability independently. However, the interactive effects of grazing legacy and resource enrichment on ecosystem multidimensional stability (e.g., temporal stability (TS): the degree of constancy of ecosystem components over time and temporal resistance (TR): the ability of ecosystem components to withstand the environmental change) in grassland ecosystems remain underexplored. In this study, we conducted a field manipulation experiment to assess the impact of 4-yr of resource addition (water and nitrogen) on multidimensional stability of multiple ecosystem components and underlying drivers in Inner Mongolia steppe with 7-yr different experimental grazing history. We found that the positive effects of water + nitrogen addition on multifunctional TS increased with increasing grazing intensity and an opposing trend was observed for multifunctional TR response. However, neither grazing legacy nor resource addition had an effect on community compositional stability. Resource addition enhanced the stability of species evenness, CWM (community weighted mean) species biomass and CWM-traits. Furthermore, water + nitrogen additions stimulated soil temperature TS but reduced its TR in heavy grazing intensity, with high grazing intensity bolstering soil moisture stability. Multifunctional stability was primarily governed by species asynchrony, while stability of species evenness fostered compositional stability. In particular, TS of functional diversity enhanced multifunctional TS in light grazing intensity, while TS of CWM-traits promoted multifunctional TS in heavy grazing intensity. Our study underscores the decoupling responses of functional stability and compositional stability to grazing legacy combined with resource enrichment. These findings highlight that the significance of concurrently considering multiple stability dimensions and components for a comprehensive understanding of grassland ecosystem stability under intensifying land use and global change scenarios.
众所周知,长期放牧和资源富集会单独影响草原生态系统的稳定性。然而,放牧遗存和资源富集对草原生态系统多维稳定性(如时间稳定性(TS):生态系统成分随时间变化的恒定程度和时间抵抗力(TR):生态系统成分抵御环境变化的能力)的交互影响仍未得到充分探索。在本研究中,我们进行了一项田间操作实验,以评估在内蒙古草原不同放牧历史的 7 年实验中,4 年的资源添加(水和氮)对生态系统多种成分的多维稳定性和潜在驱动因素的影响。我们发现,随着放牧强度的增加,水和氮的添加对多功能TS的正效应增加,而多功能TR的响应则呈相反趋势。然而,放牧历史和资源添加对群落组成的稳定性都没有影响。资源添加增强了物种均匀度、CWM(群落加权平均值)物种生物量和 CWM 特征的稳定性。此外,水和氮的添加刺激了土壤温度TS,但降低了重度放牧强度下的土壤温度TR,而高放牧强度则增强了土壤湿度稳定性。多功能稳定性主要受物种异步性的影响,而物种均匀性的稳定性则促进了成分稳定性。特别是,功能多样性的TS增强了轻度放牧强度下的多功能TS,而CWM-特征的TS则促进了重度放牧强度下的多功能TS。我们的研究强调了功能稳定性和组成稳定性对放牧遗存与资源富集的脱钩反应。这些发现突出表明,同时考虑多个稳定性维度和成分对于全面了解土地利用加剧和全球变化情景下的草原生态系统稳定性具有重要意义。
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引用次数: 0
Management and rhizosphere microbial associations modulate genetic-driven nitrogen fate 管理和根瘤微生物关联调节遗传驱动的氮归宿
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-26 DOI: 10.1016/j.agee.2024.109308
Mitra Ghotbi , Marjan Ghotbi , Yakov Kuzyakov , William R. Horwath
The interplay between plant genotype and nutrient management affects rhizodeposition, which in turn modulates the rhizosphere-microbiome and microbe-mediated functions. Substituting mineral nitrogen (N) with an N-fixing inoculant reduces reliance on N fertilizer while supplying N to crops. We evaluated the effectiveness of integrating maize near-isogenic lines (NIL 1 and NIL 2) with the biological nitrification inhibition (BNI) trait into management practices aimed at optimizing N provisioning. Management strategies included mineral N inputs (0 and 67 kg ha⁻¹) with and without an N-fixing inoculant. Our approach synthesized insights from amplicon sequencing data and evaluated nitrification rates, rhizosphere N content, maize N uptake, and N use efficiency (NUE). Genotypes and management structured prokaryotic communities, while the developmental stages of genotypes further refined both fungal and prokaryotic communities. The N-fixing inoculant increased N availability, triggering the BNI capacity without increasing the nitrification rate. This was reflected in lower NO₃⁻ and higher NH₄⁺ levels in BNI-NIL leachate compared to B73, suggesting improved N retention. NIL2, characterized by distinct fungal biomarkers, exhibited higher N content (72.3 kg ha⁻¹) and superior NUE compared to NIL1 (65.0 kg ha⁻¹). NIL2’s enhanced N uptake was associated with a robust microbial network, featuring Archangium (prokaryote) and Trichoderma (eukaryote) as keystone taxa. Notably, Archangium was linked to rhizosphere N dynamics Synergizing BNI with diazotroph inoculants reduces N fertilizer reliance and increases maize N supply for sustainable agroecosystems.
植物基因型与养分管理之间的相互作用会影响根瘤沉积,进而调节根瘤微生物群和微生物介导的功能。用固氮接种剂替代矿物氮可减少对氮肥的依赖,同时为作物提供氮。我们评估了将具有生物硝化抑制(BNI)性状的玉米近交系(NIL 1 和 NIL 2)与旨在优化氮供应的管理措施相结合的效果。管理策略包括使用或不使用固氮接种剂的矿物氮投入(0 和 67 千克/公顷-¹)。我们的方法综合了扩增子测序数据的见解,并评估了硝化率、根瘤氮含量、玉米氮吸收量和氮利用效率(NUE)。基因型和管理构建了原核生物群落,而基因型的发育阶段则进一步完善了真菌和原核生物群落。固氮接种剂提高了氮的可用性,在不增加硝化率的情况下激发了 BNI 能力。与 B73 相比,BNI-NIL 浸出液中的 NO₃- 含量更低,NH₄⁺ 含量更高,这表明氮的保留得到了改善。与 NIL1(65.0 千克/公顷-¹)相比,NIL2 的氮含量更高(72.3 千克/公顷-¹),氮利用率更高(65.0 千克/公顷-¹)。NIL2 对氮的吸收增强与强大的微生物网络有关,其特点是以 Archangium(原核生物)和 Trichoderma(真核生物)为关键类群。值得注意的是,弓形菌与根瘤层氮的动态有关 将 BNI 与重氮营养体接种剂协同作用,可减少对氮肥的依赖,增加玉米氮供应,实现可持续的农业生态系统。
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引用次数: 0
Warming, elevated CO2 and drought in combination amplify shifts in canopy greenness dynamics in managed grassland 气候变暖、二氧化碳升高和干旱共同加剧了受管理草地冠层绿度动态的变化
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-26 DOI: 10.1016/j.agee.2024.109304
Lumnesh Swaroop Kumar Joseph , Edoardo Cremonese , Mirco Migliavacca , Andreas Schaumberger , Michael Bahn
Grasslands are strongly exposed to multiple global changes, including elevated CO2, warming, and severe drought events. While the individual effects of these global change drivers on the greenness dynamics of grasslands have been comparatively well studied, their combined effects are so far poorly understood. In an in situ multifactor experiment we tested the individual and combined effects of warming (+3° C), elevated CO2 atmospheric concentration (+300 ppm) and summer drought on the spring phenology and regrowth dynamics following defoliation during summer and late summer of a managed grassland typical for many parts of the Alps. We derived the dynamics of canopy greenness from the time series of green chromatic coordinates using digital repeat photography imagery (phenocams) spanning a period of three years. Among the individual drivers tested, we found that warming strongly advanced spring phenology and accelerated growth, elevated CO2 accelerated growth, and summer drought had no immediate effects on shifts in canopy greenness but accelerated growth in the subsequent spring. The combination of the three global change drivers caused the most pronounced spring phenological and regrowth dynamics among all treatments, triggering an earlier reduction in canopy greenness during summer and advancing the onset of growth in the successive spring due to a drought legacy effect, which decreased the cumulative growing degree days required for initiating growth. Our findings suggest that in a future climate the combined effects of the three global change drivers will exacerbate shifts in canopy greenness dynamics in managed grassland, which cannot be predicted from the responses from the individual effects of these drivers.
草原深受多种全球变化的影响,包括二氧化碳升高、气候变暖和严重干旱事件。虽然这些全球变化驱动因素对草地绿化动态的单独影响已经得到了比较充分的研究,但迄今为止,人们对它们的综合影响还知之甚少。在一项原位多因素实验中,我们测试了气候变暖(+3° C)、大气中二氧化碳浓度升高(+300 ppm)和夏季干旱对阿尔卑斯山许多地区典型的管理草地夏季和夏末落叶后的春季物候和再生动态的单独和综合影响。我们利用数字重复摄影图像(phenocams)从绿色色度坐标的时间序列中得出了树冠绿色度的动态变化,时间跨度为三年。在测试的单个驱动因素中,我们发现气候变暖会强烈推进春季物候期并加速生长,二氧化碳升高会加速生长,而夏季干旱对树冠绿色度的变化没有直接影响,但会加速随后春季的生长。在所有处理中,三种全球变化驱动因素的组合造成了最明显的春季物候和再生动态变化,在夏季引发了树冠绿色度的提前减少,并由于干旱遗留效应(减少了开始生长所需的累积生长度日)而使随后春季的生长开始时间提前。我们的研究结果表明,在未来的气候条件下,三种全球变化驱动因素的综合效应将加剧受管理草地冠层绿度动态的变化,而这种变化是无法从这些驱动因素的单独效应中预测出来的。
{"title":"Warming, elevated CO2 and drought in combination amplify shifts in canopy greenness dynamics in managed grassland","authors":"Lumnesh Swaroop Kumar Joseph ,&nbsp;Edoardo Cremonese ,&nbsp;Mirco Migliavacca ,&nbsp;Andreas Schaumberger ,&nbsp;Michael Bahn","doi":"10.1016/j.agee.2024.109304","DOIUrl":"10.1016/j.agee.2024.109304","url":null,"abstract":"<div><div>Grasslands are strongly exposed to multiple global changes, including elevated CO<sub>2</sub>, warming, and severe drought events. While the individual effects of these global change drivers on the greenness dynamics of grasslands have been comparatively well studied, their combined effects are so far poorly understood. In an <em>in situ</em> multifactor experiment we tested the individual and combined effects of warming (+3° C), elevated CO<sub>2</sub> atmospheric concentration (+300 ppm) and summer drought on the spring phenology and regrowth dynamics following defoliation during summer and late summer of a managed grassland typical for many parts of the Alps. We derived the dynamics of canopy greenness from the time series of green chromatic coordinates using digital repeat photography imagery (phenocams) spanning a period of three years. Among the individual drivers tested, we found that warming strongly advanced spring phenology and accelerated growth, elevated CO<sub>2</sub> accelerated growth, and summer drought had no immediate effects on shifts in canopy greenness but accelerated growth in the subsequent spring. The combination of the three global change drivers caused the most pronounced spring phenological and regrowth dynamics among all treatments, triggering an earlier reduction in canopy greenness during summer and advancing the onset of growth in the successive spring due to a drought legacy effect, which decreased the cumulative growing degree days required for initiating growth. Our findings suggest that in a future climate the combined effects of the three global change drivers will exacerbate shifts in canopy greenness dynamics in managed grassland, which cannot be predicted from the responses from the individual effects of these drivers.</div></div>","PeriodicalId":7512,"journal":{"name":"Agriculture, Ecosystems & Environment","volume":"378 ","pages":"Article 109304"},"PeriodicalIF":6.0,"publicationDate":"2024-09-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142322562","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
Optimizing phosphate application to improve soil quality and reduce phosphorus loss in rice-wheat rotation 优化磷肥施用,改善土壤质量,减少水稻-小麦轮作中的磷流失
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-26 DOI: 10.1016/j.agee.2024.109310
Guanglei Chen , Liang Xiao , Ke Yue , Yu Wang , Shenqiang Wang , Yiyong Zhu , Lei Kai
How to determine the optimal dosage of phosphorus (P) fertilizer input for an agricultural field is important to maintain soil quality and crop production while minimizing environmental impact. In this study, we set up a 5-year rice-wheat rotation with contrasting P fertilization treatments (0, 25, 50, 75, 100, and 150 kg P2O5 ha−1, hereafter, P0, P25, P50, P75, P100, and P150, respectively) per season to explore the relationship between the amount of P input and crop yield, P use efficiency (PUE), balance of P accumulation and loss, ecosystem multifunctionality (EMF), and soil quality. Our results indicate that increased P amounts significantly boosted rice and wheat production of both straw and grain, but the tendency slowed down when the input was over 75 kg P2O5 ha−1. The PUE declined with increased P input and soil P balance of 50 kg P2O5 ha−1 for wheat and 100 kg P2O5 ha−1 for rice. Runoff emerges as the main pathway for soil P loss and escalates with higher P application rates. We emphasize increasing ridge height and controlling water input for basal fertilizer to minimize P loss. The application of P fertilizer increased the soil P pool, with labile P (L-P) and moderately labile P (M-P) increasing by 13–114 % and 23–111 %, respectively, compared to P0. The transformation of M-P to L-P in paddy soil is associated with an increased abundance of Actinobacteria. Low P applications (P25 and P50) increased EMF by 3.27 and 3.58 times, while high P applications (P75, P100, and P150) decreased EMF. Furthermore, P application significantly improved the soil quality index (SQI) compared to P0. The impact of abiotic factors on yield and P loss is more significant than that of biotic elements, with the SQI serving as a dependable indicator for predicting yield. Central to minimizing P loss while maximizing yield is the reduction of Resin-P content and the maintenance of NaOH-Pi levels, suggesting that organic materials may be a good alternative strategy. These findings provide valuable data and theoretical support for optimizing P application in rice-wheat cropping systems, promoting a mutually beneficial scenario for agricultural production and ecological protection.
如何确定农田磷肥的最佳施用量,对于保持土壤质量和作物产量,同时最大限度地减少对环境的影响非常重要。在本研究中,我们设置了一个为期 5 年的稻麦轮作期,每季施用不同的磷肥处理(分别为 0、25、50、75、100 和 150 kg P2O5 ha-1,以下简称 P0、P25、P50、P75、P100 和 P150),以探讨磷肥施用量与作物产量、磷肥利用效率(PUE)、磷肥积累和流失平衡、生态系统多功能性(EMF)和土壤质量之间的关系。我们的研究结果表明,增加钾的用量能显著提高水稻和小麦的秸秆和谷物产量,但当钾的投入量超过 75 kg P2O5 ha-1 时,这一趋势就会放缓。小麦的 PUE 随 P 投入量的增加而下降,土壤 P 平衡为 50 kg P2O5 ha-1,水稻为 100 kg P2O5 ha-1。径流是土壤钾流失的主要途径,并且随着钾施用量的增加而增加。我们强调增加田埂高度和控制基肥的进水量,以尽量减少钾的流失。施用钾肥增加了土壤钾库,与钾肥施用量为 0 时相比,可溶性钾(L-P)和中度可溶性钾(M-P)分别增加了 13-114 % 和 23-111 %。稻田土壤中 M-P 向 L-P 的转化与放线菌数量的增加有关。施用低浓度磷(P25 和 P50)会使 EMF 增加 3.27 倍和 3.58 倍,而施用高浓度磷(P75、P100 和 P150)会使 EMF 减少。此外,与 P0 相比,施用 P 能明显改善土壤质量指数(SQI)。非生物因素对产量和钾流失的影响比生物因素更为显著,而 SQI 则是预测产量的可靠指标。在最大限度地提高产量的同时最大限度地减少钾损失的关键是降低树脂-钾含量和保持 NaOH-钾水平,这表明有机材料可能是一种很好的替代策略。这些发现为优化水稻-小麦种植系统中的钾施用提供了宝贵的数据和理论支持,促进了农业生产和生态保护的互利共赢。
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引用次数: 0
Grazing intensity by sheep affects spatial diversity in botanical composition of Inner Mongolian grassland 羊的放牧强度影响内蒙古草原植物组成的空间多样性
IF 6 1区 农林科学 Q1 AGRICULTURE, MULTIDISCIPLINARY Pub Date : 2024-09-26 DOI: 10.1016/j.agee.2024.109311
Xu Han , Raúl Ochoa-Hueso , Yong Ding , Xiliang Li , Ke Jin , Wim H. van der Putten , Paul C. Struik
Overgrazing by sheep causes degradation of grasslands in the Inner Mongolian steppe, yet our understanding of its impact on grassland plant communities is limited by lack of observations at high spatial resolution. Employing a nested experimental design in a long-term grazing experiment provides insights into effects of increasing sheep grazing intensity on community composition, diversity, and spatial patterns in the grassland vegetation. Effects of observed changes in the plant community are discussed based on monthly weight gain of sheep during grazing. The design of the long-term experiment included four triplicated grazing intensities applied during an 8-year period. At the end of that period, we evaluated vegetation coverage, categorized plant species by functional groups, and analyzed the data using a mixed linear model. Moreover, spatial autocorrelation methods were employed to investigate spatial patterns, visualized via a kriging model. We found that the plant community composition differed among grazing treatments, with high grazing intensity showing higher plant species richness and stronger clustering of plants at our fine scale of observation. These fine-grained spatial scale observations are usually not recorded in larger spatial scale analyses of grassland responses to overgrazing. While the grazing intensities used in our study did not influence individual sheep weight gain, total sheep weight gain per hectare increased with an increase in grazing intensity. Our study shows that in a sheep grazing intensity experiment in Inner Mongolia grasslands total sheep weight gain may increase at the expense of fine-scale species composition and spatial dynamics of the grassland vegetation. These insights may be used for determining trade-offs of sheep meat production with original composition and structure of grassland plant communities. Effects on other ecosystem properties and functions, such as on belowground biodiversity, remain to be assessed.
绵羊过度放牧导致内蒙古草原退化,但由于缺乏高空间分辨率的观测,我们对绵羊过度放牧对草原植物群落的影响的了解十分有限。通过在长期放牧实验中采用嵌套实验设计,我们可以深入了解羊群放牧强度的增加对草原植被群落组成、多样性和空间模式的影响。根据放牧期间绵羊的月增重情况,讨论了观察到的植物群落变化的影响。长期实验的设计包括在 8 年时间里采用四种三倍的放牧强度。实验结束后,我们对植被覆盖率进行了评估,按功能群对植物物种进行了分类,并使用混合线性模型对数据进行了分析。此外,我们还采用了空间自相关方法来研究空间模式,并通过克里金模型将其可视化。我们发现,在不同的放牧处理中,植物群落组成有所不同,放牧强度越高,植物物种的丰富度越高,在我们的精细观测尺度上,植物的聚类越强。这些细粒度空间尺度的观测结果通常不会记录在草原对过度放牧反应的较大空间尺度分析中。虽然我们研究中使用的放牧强度并不影响绵羊的个体增重,但绵羊每公顷的总增重却随着放牧强度的增加而增加。我们的研究表明,在内蒙古草原进行的绵羊放牧强度试验中,绵羊总增重的增加可能会以草原植被的精细物种组成和空间动态为代价。这些见解可用于确定绵羊肉产量与草原植物群落原始组成和结构之间的权衡。对其他生态系统特性和功能的影响,如对地下生物多样性的影响,仍有待评估。
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引用次数: 0
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Agriculture, Ecosystems & Environment
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