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Drivers of soil quality and maize yield under long-term tillage and straw incorporation in Mollisols 莫利土壤中长期耕作和秸秆掺入条件下土壤质量和玉米产量的驱动因素
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-16 DOI: 10.1016/j.still.2024.106360
Chunzhu Liu , Bingcheng Si , Ying Zhao , Zhimin Wu , Xinchun Lu , Xu Chen , Xiaozeng Han , Yuanchen Zhu , Wenxiu Zou
Proper tillage combined with straw management is crucial for maintaining agroecosystem sustainability and crop yield, especially under intensified agricultural activities. However, the optimal depth for tillage in combination with straw incorporation remains unclear. To address this, we established a field experiment in 2011 in Mollisols with five treatments: conventional tillage (CT, tillage depth 20 cm), no-tillage combined with straw return (SNT), conventional tillage combined with straw return (SCT), inversion tillage combined with straw return (SIT, tillage depth 35 cm), and subsoil tillage combined with straw return (SST, straw depth 20–35 cm). We assessed the effects of these treatments on soil quality by evaluating the Soil Physical Property Index (SPI), Soil Chemical Property Index (SCI), and Soil Microbial Property Index (SMI) in relation to the Soil Quality Index (SQI) and crop yield. Our findings shown that tillage combined with straw return significantly improved soil properties. Compared to the CT, SNT, and SST treatments, the SCT and SIT treatments increased SPI and SQI in the 0–20 cm soil layer by 43.9–845.4 %. While the SIT and SST treatments enhanced SPI, SCI, and SMI in the 20–35 cm soil layer by 69.2–307.7 % more than the CT, SNT, and SCT treatments. Among all treatments, SIT treatment resulted in the highest SPI, SCI, and SMI in the 0–35 cm soil layer. Additionally, SQI and maize yield under the SIT treatment were 11.7–140.5 % and 15.6–78.0 % higher, respectively, compared to other treatments. Linear regression analysis revealed that SPI in all layers had a significant impact on maize yield, while SCI and SMI were significantly correlated with yield only in the 20–35 cm layer (P < 0.05). SPI's contribution to maize yield was 18.6–156.8 % higher than that of SCI and SMI. Partial least-squares path modeling identified SPI as a direct influence on SMI and SCI, making it the largest driver indirectly improving SQI and maize yield in Mollisols. Therefore, SIT treatment is a highly effective soil management practice for improving soil quality and crop yields in the Mollisols region. Our study provides guidance for enhancing soil environmental quality and designing sustainable agricultural policies in the Mollisols region and other arable soils.
适当的耕作结合秸秆管理对于保持农业生态系统的可持续性和作物产量至关重要,尤其是在强化农业活动的情况下。然而,结合秸秆还田的最佳耕作深度仍不明确。为了解决这个问题,我们于 2011 年在莫利土壤中进行了一项田间试验,共采用了五种处理:常规耕作(CT,耕作深度 20 厘米)、免耕结合秸秆还田(SNT)、常规耕作结合秸秆还田(SCT)、反转耕作结合秸秆还田(SIT,耕作深度 35 厘米)和底土耕作结合秸秆还田(SST,秸秆深度 20-35 厘米)。我们通过评估土壤物理属性指数(SPI)、土壤化学属性指数(SCI)和土壤微生物属性指数(SMI)与土壤质量指数(SQI)和作物产量的关系,评估了这些处理对土壤质量的影响。我们的研究结果表明,耕作结合秸秆还田能显著改善土壤性质。与 CT、SNT 和 SST 处理相比,SCT 和 SIT 处理使 0-20 厘米土层的 SPI 和 SQI 提高了 43.9%-845.4%。与 CT、SNT 和 SCT 相比,SIT 和 SST 处理提高了 20-35 厘米土层的 SPI、SCI 和 SMI,增幅为 69.2-307.7 %。在所有处理中,SIT 处理使 0-35 厘米土层的 SPI、SCI 和 SMI 最高。此外,与其他处理相比,SIT 处理的 SQI 和玉米产量分别高出 11.7-140.5 % 和 15.6-78.0 %。线性回归分析表明,所有土层的 SPI 对玉米产量都有显著影响,而 SCI 和 SMI 仅在 20-35 厘米土层与产量有显著相关性(P < 0.05)。SPI 对玉米产量的贡献比 SCI 和 SMI 高 18.6-156.8 %。偏最小二乘路径模型确定 SPI 对 SMI 和 SCI 有直接影响,使其成为间接提高 SQI 和 Mollisols 玉米产量的最大驱动力。因此,SIT 处理是提高土壤质量和作物产量的一种非常有效的土壤管理方法。我们的研究为提高莫里索地区和其他耕地的土壤环境质量和设计可持续农业政策提供了指导。
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引用次数: 0
Significant increases in nitrous oxide emissions under simulated extreme rainfall events and straw amendments from agricultural soil 在模拟极端降雨事件和农业土壤秸秆改良的情况下,一氧化二氮排放量显著增加
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-14 DOI: 10.1016/j.still.2024.106361
Xiaogang Li , Rui Wang , Yanling Du , Hui Han , Shengli Guo , Xiaotong Song , Xiaotang Ju
Pulsed N2O emissions resulting from field management practices (N fertilization addition and straw return) or rainfall events make for a significant proportion of the total annual N2O budget from croplands. However, it remains unclear whether altered rainfall patterns induced by climate change will stimulate the responses of pulsed N2O emissions to various field practices. In this study, we aimed to elucidate the underlying mechanisms driving pulsed N2O emissions in response to extreme rainfall events and examine their interaction with carbon and nitrogen availability. We hypothesized that highly available substrates rapidly induce an anaerobic environment and N2O pulses during extreme rainfall events. A soil column experiment under simulating extreme rainfall events was conducted to investigate the responses of pulsed N2O emissions to three common farming practices: nitrogen fertilization (N), nitrogen fertilization coupled with low straw return (N+LS), and nitrogen fertilization coupled with high straw return (N+HS). We frequently monitored surface emissions and soil concentrations of N2O and CO2, and measured O2, NH4+, NO3- and DOC concentrations. N and straw amendments together under simulated rainfall events significantly depleted O2, and simultaneously increased pulsed N2O emissions. The N+HS treatment exhibited the highest soil N2O concentration (51.9 µL L−1) and lowest O2 concentration (4.3 %), along with high soil moisture levels (24.8 %–32.2 %). Correspondingly, the highest cumulative N2O emissions were observed in the N+HS treatment (117.8 mg m−2), followed by 52.2, 31.9, and 11.0 mg m−2 for the N+LS, N, and CK treatments, respectively. The promotion of N2O production by highly available substrates confirms our hypothesis. Our work contributes to the refinement of global climate models and field mitigation practices, as pulsed N2O emissions from croplands will increase under future extreme rainfall events owing to climate change.
田间管理措施(氮肥添加和秸秆还田)或降雨事件导致的脉冲式一氧化二氮排放占农田年度一氧化二氮总预算的很大一部分。然而,气候变化引起的降雨模式改变是否会刺激脉冲 N2O 排放对各种田间管理措施的响应,目前仍不清楚。在这项研究中,我们旨在阐明驱动脉冲式一氧化二氮排放以应对极端降雨事件的基本机制,并研究它们与碳和氮可用性之间的相互作用。我们假设,在极端降雨事件中,高可用基质会迅速诱发厌氧环境和 N2O 脉冲。我们在模拟极端降雨事件的土壤柱实验中,研究了脉冲 N2O 排放对三种常见耕作方式的响应:氮肥(N)、氮肥与低秸秆还田(N+LS)和氮肥与高秸秆还田(N+HS)。我们经常监测 N2O 和 CO2 的地表排放和土壤浓度,并测量 O2、NH4+、NO3- 和 DOC 的浓度。在模拟降雨情况下,氮和秸秆一起施用会显著消耗氧气,同时增加脉冲式一氧化二氮排放。N+HS 处理的土壤 N2O 浓度最高(51.9 µL L-1),O2 浓度最低(4.3%),土壤湿度也较高(24.8%-32.2%)。相应地,N+HS 处理的累积 N2O 排放量最高(117.8 mg m-2),其次是 N+LS、N 和 CK 处理,分别为 52.2、31.9 和 11.0 mg m-2。高可利用基质对 N2O 生成的促进作用证实了我们的假设。我们的研究有助于完善全球气候模型和田间减排实践,因为在未来气候变化导致的极端降雨事件中,耕地的脉冲式一氧化二氮排放将会增加。
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引用次数: 0
Straw incorporating in shallow soil layer improves field productivity by impacting soil hydrothermal conditions and maize reproductive allocation in semiarid east African Plateau 将秸秆掺入浅土层可影响半干旱东非高原的土壤水热条件和玉米生殖分配,从而提高田间生产力
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-14 DOI: 10.1016/j.still.2024.106351
Sylvia Ngaira Indoshi , Wesly Kiprotich Cheruiyot , Muhammad Maqsood Ur Rehman , Fu-Jian Mei , Qing-Hui Wen , Alex Ndolo Munyasya , Kiprotich Koskei , David Mwehia Mburu , Aggrey Bernard Nyende , Levis Kavagi , Delphine Nyanchera Gisacho , Eliyas Feyisa Sori , Yi-Bo Wang , Hong-Yan Tao , You-Cai Xiong
Ridge-furrow plastic film mulching (RFM) planting system can conserve soil water and boost crop yield in semi-arid rainfed agricultural areas. In the east African Plateau (EAP), the RFM system has shown significant promoting effects on the yield and water use efficiency in maize (Zea mays L.) and wheat (Triticum aestivum L.). Although the RFM system is effective and efficient, it is unclear how to further increase crop productivity under RFM in EAP where soil moisture is limited. This study advocates for an integrated practice (maize straw returning) in the RFM system. Field trials were conducted using maize cultivar DK8031 to investigate the effects of maize straw returning in the shallow soil layer on soil hydrothermal conditions from 2021 to 2022. Maize productivity, water use efficiency, soil organic carbon, and soil total nitrogen were determined under RFM in Kenya, EAP. Three treatments were designed as follows: 1) conventional bare flat planting, CK; 2) RF with full plastic film mulching, RFM; and 3) RFM with maize straw piece (9 t ha−1) returning to 0–30 cm soil layer, RFMR. The results indicated that soil water storage (SWS) was substantially improved by 40.8 mm in 2021 and 30.9 mm in 2022 in RFMR, respectively, than that of CK, which was also significantly greater than that of RFM (p<0.05). Under relatively high air temperature at the silking stage, soil temperature at 15 cm soil depth was averagely reduced by 0.85 °C in RFMR and 0.15 °C in RFM, respectively, compared with CK. Across two growing seasons, grain yield and water use efficiency increased by 470 kg ha−1 and 1.5 kg ha−1mm−1 in RFMR compared to RFM and 2407 kg ha−1 and 7.1 kg ha−1mm−1 compared with CK, respectively., The highest economic benefit was found in RMFR, relative to RFM and CK. The above trend was positively associated with the improvements in hydrothermal conditions in the shallow soil layer. Additionally, soil organic carbon was increased by 0.88 g kg−1 in RFMR relative to CK due to improved soil structure and physiochemical traits. For the first time, we found that straw pieces returning to the shallow soil layer can further boost maize productivity on the basis of RFM, which was intended to improve soil texture in EAP.
脊-沟塑料薄膜覆盖(RFM)种植系统可以在半干旱雨水灌溉农业地区保持土壤水分并提高作物产量。在东非高原(EAP),RFM 系统对玉米(Zea mays L.)和小麦(Triticum aestivum L.)的产量和水分利用效率有显著的促进作用。虽然 RFM 系统效果显著、效率高,但在土壤水分有限的东亚和太平洋地区,如何在 RFM 系统下进一步提高作物产量尚不清楚。本研究提倡在 RFM 系统中采用综合做法(玉米秸秆还田)。在 2021 年至 2022 年期间,使用玉米栽培品种 DK8031 进行了田间试验,研究浅土层玉米秸秆还田对土壤水热条件的影响。测定了肯尼亚东亚农业区 RFM 下的玉米生产力、水分利用效率、土壤有机碳和土壤全氮。设计了以下三个处理:1)常规裸地种植,CK;2)全塑料薄膜覆盖的 RF,RFM;3)玉米秸秆片(9 吨/公顷-1)覆盖 0-30 厘米土层的 RFM,RFMR。结果表明,RFMR 在 2021 年和 2022 年的土壤蓄水量(SWS)分别比 CK 显著提高了 40.8 毫米和 30.9 毫米(p<0.05)。在吐丝期气温相对较高的情况下,RFMR 和 RFM 15 厘米土层深度的土壤温度分别比 CK 平均降低了 0.85 °C和 0.15 °C。在两个生长季中,与 RFM 相比,RFMR 的谷物产量和水分利用效率分别增加了 470 千克/公顷和 1.5 千克/公顷-1 毫米-1;与 CK 相比,RFMR 的谷物产量和水分利用效率分别增加了 2407 千克/公顷和 7.1 千克/公顷-1 毫米-1。上述趋势与浅土层水热条件的改善呈正相关。此外,由于土壤结构和理化性状的改善,相对于 CK,RFMR 的土壤有机碳增加了 0.88 g kg-1。我们首次发现,在 RFM 的基础上,秸秆碎片回归浅土层可进一步提高玉米产量,从而改善 EAP 的土壤质地。
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引用次数: 0
Improving the accuracy of soil organic matter mapping in typical Planosol areas based on prior knowledge and probability hybrid model 基于先验知识和概率混合模型提高典型 Planosol 地区土壤有机质绘图的准确性
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-14 DOI: 10.1016/j.still.2024.106358
Deqiang Zang , Yinghui Zhao , Chong Luo , Shengqi Zhang , Xilong Dai , Yong Li , Huanjun Liu
The use of remote sensing techniques for mapping soil organic matter (SOM) in black soil regions is well established. However, in areas where Planosols are interspersed with non-Planosols, tilling impacts the soil spectra of tilled soils at varying times and to different extents. As a result, errors may arise when modeling Planosols and non-Planosols collectively using conventional methods. This study developed a probability hybrid model specifically designed for the interlayered zones of Planosol and non-Planosol soils to accurately reflect the content and spatial distribution of SOM. A total of 712 topsoil samples were collected from the 852 Farm, a typical area with the interlayered zones of Planosol and non-Planosol soils in northeastern China. Cloud-free Sentinel-2 images were obtained during the bare soil period from April to May between 2021 and 2023. The spatial distribution of Planosol was detected, and the probability of soil classification was calculated using a random forest model. Based on soil classification probabilities, global models, multi-temporal ordinary hybrid models, and multi-temporal probability hybrid models were developed respectively. The results of SOM mapping using these different strategies were compared. Under seasonal reductive leaching, Planosol exhibits a distinct eluvial horizon beneath the topsoil. Long-term tilling leads to the mixing of this eluvial horizon with the topsoil in Planosol, resulting in spectral characteristics that differ significantly from those of other soil types. Accordingly, we propose a new remote sensing index—the Normalized Difference Planosol Index (NDPI), to reflect the upturning degree of the eluvial horizon and get “whiteness degree” information. We evaluated the effect of adding this index as an input on the detection of Planosol and the accuracy of SOM mapping. The results of the study show that (1) May is the optimal time window for SOM mapping and Planosol detection in the typical interlayered area of Planosol and non-Planosol soils. (2) Based on the random forest model combined with multi-period May bare soil images can accurately detect the spatial distribution of Planosol with the highest accuracy, the overall accuracy is 97.66 %; (3) The hybrid models outperform the global model, with the probability hybrid model achieving the highest accuracy (R2=0.8056, RMSE=4.2869 g/kg) and the mapping is more continuous and smoother. (4) The inclusion of NDPI improves the accuracy of Planosol spatial distribution detection and SOM mapping in Planosol areas, resulting in an increase in the Kappa coefficient by 0.0168 and an improvement in R2 by 0.0122. The present study innovatively utilizes remote sensing imagery to monitor Planosol, thus expanding the application of remote sensing technology in digital soil mapping.
利用遥感技术绘制黑土区土壤有机质(SOM)图的做法已得到广泛认可。然而,在浮土与非浮土交错的地区,翻耕会在不同时间和不同程度上影响翻耕土壤的土壤光谱。因此,使用传统方法对浮土和非浮土进行综合建模时可能会出现误差。本研究开发了一种概率混合模型,专门用于 Planosol 和非 Planosol 土壤的夹层区,以准确反映 SOM 的含量和空间分布。在中国东北典型的浮土与非浮土交错带地区--八五二农场,共采集了 712 个表层土样本。在 2021 年至 2023 年期间的 4 月至 5 月裸土期获取了无云哨兵-2 图像。检测了浮土的空间分布,并利用随机森林模型计算了土壤分类的概率。根据土壤分类概率,分别建立了全局模型、多时相普通混合模型和多时相概率混合模型。比较了使用这些不同策略绘制 SOM 图的结果。在季节性还原沥滤作用下,Planosol 表层土下有明显的冲积层。长期翻耕会导致冲积层与 Planosol 表层土混合,从而产生与其他土壤类型明显不同的光谱特征。因此,我们提出了一种新的遥感指数--归一化差异普朗索指数(NDPI),以反映冲积层的上翻程度,获得 "白度 "信息。我们评估了添加该指数作为输入对 Planosol 检测和 SOM 制图精度的影响。研究结果表明:(1)在典型的浮土与非浮土交错区域,5 月是 SOM 制图和浮土检测的最佳时间窗。(2)基于随机森林模型结合多期 5 月裸露土壤图像可准确地探测到 Planosol 的空间分布,准确率最高,总体准确率为 97.66%;(3)混合模型优于全局模型,其中概率混合模型的准确率最高(R2=0.8056,RMSE=4.2869 g/kg),且绘图更连续、更平滑。(4)NDPI 的加入提高了 Planosol 空间分布检测和 Planosol 区域 SOM 绘图的精度,使 Kappa 系数提高了 0.0168,R2 提高了 0.0122。本研究创新性地利用遥感图像监测 Planosol,从而拓展了遥感技术在数字土壤制图中的应用。
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引用次数: 0
Improved soil organic matter monitoring by using cumulative crop residue indices derived from time-series remote sensing images in the central black soil region of China 利用时间序列遥感图像得出的作物残留累积指数改进中国中部黑土区土壤有机质监测工作
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-13 DOI: 10.1016/j.still.2024.106357
Mei-Wei Zhang , Xiao-Lin Sun , Mei-Nan Zhang , Hao-Xuan Yang , Huan-Jun Liu , Hou-Xuan Li
Soil organic matter (SOM) determines soil fertility and functions, playing a key role in agriculture, the environment and climate change. During the past century, the SOM of the world, e.g., the black soil (Mollisol) in croplands of Northeast China, experienced extensive changes, making SOM monitoring crucial. Recently, digital soil mapping (DSM) with time-series remote sensing images has become a mainstream method for SOM monitoring, but there is room for its accuracy to be improved. To fulfill this purpose, we propose utilizing crop residue indices (CRIs) derived from remote sensing images within the method, as crop residues are a main source of the SOM. In this study, performances of five commonly used CRIs, e.g., normalized difference tillage index (NDTI), on SOM monitoring was evaluated based on a series of topsoil samples collected from 2014 to 2018 in croplands of the center black soil region in Northeast China. The performances and those of cumulative CRIs computed over some years were compared to those of basic climate and terrain attributes, spectral bands, an empirical index, and commonly used vegetation indices (VIs, e.g., normalized difference vegetation index (NDVI)). Results showed that temporal CRIs had a stronger correlation with SOM content (0.52–0.73) than did the others (0.04–0.69). Integrating CRIs with basic soil covariates increased prediction accuracy by 7.27 % in Lin’s concordance correlation coefficient (CCC). Further, the CRIs and VIs accumulated over 3 and 4 years, respectively, had a much stronger correlation with SOM (0.65–0.73 and 0.67–0.69, respectively) and led to better accuracies with an average increase of 2.62 % in CCC compared to indices of the current sampling year. While annual SOM maps predicted with and without the optimal cumulative CRI showed similar spatial patterns, they were statistically significantly different. It is recommended to utilize the cumulative NDTI for monitoring SOM.
土壤有机质(SOM)决定着土壤的肥力和功能,在农业、环境和气候变化中发挥着关键作用。在过去的一个世纪中,全球的土壤有机质(如中国东北耕地的黑土(Mollisol))经历了巨大的变化,因此土壤有机质的监测至关重要。近年来,利用时间序列遥感图像绘制数字土壤图(DSM)已成为 SOM 监测的主流方法,但其精度还有待提高。为了实现这一目标,我们建议在该方法中使用从遥感图像中提取的作物残留物指数(CRIs),因为作物残留物是 SOM 的主要来源。本研究基于 2014 年至 2018 年在中国东北黑土中心区耕地采集的一系列表土样本,评估了归一化差异耕作指数(NDTI)等五种常用 CRIs 在 SOM 监测中的表现。比较了若干年内计算的累积CRIs与基本气候和地形属性、光谱波段、经验指数以及常用植被指数(VIs,如归一化差异植被指数(NDVI))的性能和表现。结果表明,与其他指数(0.04-0.69)相比,时间 CRI 与 SOM 含量(0.52-0.73)具有更强的相关性。根据林氏一致性相关系数 (CCC),将 CRIs 与基本土壤协变量整合后,预测精度提高了 7.27%。此外,分别经过 3 年和 4 年积累的 CRIs 和 VIs 与 SOM 的相关性更强(分别为 0.65-0.73 和 0.67-0.69),与当前采样年的指数相比,CCC 平均提高了 2.62%,从而提高了预测精度。虽然使用和不使用最佳累积中分辨率预测的年度 SOM 图显示出相似的空间模式,但它们在统计上有显著差异。建议利用累积 NDTI 监测 SOM。
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引用次数: 0
Soil mineral–associated organic carbon fraction maintains quantitatively but not biochemically after cropland abandonment 耕地废弃后,土壤矿物相关有机碳部分在数量上保持不变,但在生物化学方面却没有变化
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-13 DOI: 10.1016/j.still.2024.106355
Bin Jia , Yanmei Liang , Xiaoming Mou , Han Mao , Li Jia , Jie Chen , Kuzyakov Yakov , Xiao Gang Li
Abandonment is a strategy applied to increase soil organic C (SOC) in degraded cropland, but such efforts may fail because of microbial N limitation after abandonment in the absence of fertilization. In this study, we investigated the associations between SOC and microbial necromass C (MNC) dynamics in bulk soil and particle-size pools with N availability in a cropland abandonment chronosequence on the Loess Plateau. The total SOC, total MNC, and their particulate fractions (> 0.05 mm) in soil declined in the first eight years after cropland abandonment, but increased thereafter. By the 23rd year, the SOC content in abandoned soils increased towards the levels of cropland (16.5 g kg–1) but were still far lower than those of natural vegetation (21.5 g kg–1). The mineral–associated SOC (< 0.05 mm) content maintained after abandonment; but by contrast, the mineral-associated MNC profoundly decreased. This indicated that the reduction in MNC in this fraction was compensated for by plant-derived substances from the particulate fraction. Enzymatic stoichiometry analysis identified microbial N limitations in abandoned soils compared with cropland soils. As such, microbial N limitation led to increases in mineralization and/or decreases in synthesis of MNC in both particulate and mineral-associated fractions after abandonment, attributable to the decreased total SOC. Across the abandonment chronosequence, up to 20 % of particulate SOC was derived from microbes, whereas more than half of mineral-associated SOC came from plants. These findings challenge the general consensus that particulate SOC is dominated by plant residues whereas the mineral-associated fraction contains mainly microbially derived substances. The MNC contained a smaller proportion of fungal substances in mineral-associated fractions compared to particulate fractions, reflecting microbial ecological niche differentiation in the SOC formation between particle-size fractions. In conclusion, cropland abandonment decreased MNC accumulation because of microbial N limitation, and the mineral-associated SOC was stable in quantity but not in its source composition.
弃耕是在退化的耕地中增加土壤有机碳(SOC)的一种策略,但这种努力可能会失败,因为在没有施肥的情况下,弃耕后微生物会受到氮的限制。在这项研究中,我们调查了黄土高原耕地撂荒时序中大块土壤和颗粒大小池中的 SOC 和微生物坏死物质 C(MNC)动态与氮供应之间的关系。耕地撂荒后的前八年,土壤中的总 SOC、总 MNC 及其颗粒部分(0.05 毫米)有所下降,但随后有所上升。到第 23 年,弃耕土壤中的 SOC 含量上升至耕地水平(16.5 g kg-1),但仍远低于天然植被(21.5 g kg-1)。弃耕后,与矿物相关的 SOC(< 0.05 mm)含量保持不变;但与此相反,与矿物相关的 MNC 却大幅减少。这表明,该部分中 MNC 的减少被微粒部分的植物衍生物质所补偿。酶促化学计量分析发现,与耕地土壤相比,弃耕土壤中的微生物氮含量有限。因此,微生物的氮限制导致弃耕后颗粒和矿物相关组分中 MNC 矿化增加和/或合成减少,这归因于总 SOC 的减少。在整个弃耕时间序列中,多达 20% 的微粒 SOC 来自微生物,而一半以上的矿物相关 SOC 来自植物。这些发现对颗粒 SOC 以植物残留物为主,而矿物相关部分主要包含微生物衍生物质这一普遍共识提出了质疑。与颗粒部分相比,MNC 的矿物相关部分中真菌物质所占比例较小,这反映了不同粒径部分在 SOC 形成过程中的微生物生态位差异。总之,由于微生物的氮限制,耕地弃耕减少了 MNC 的积累,与矿物相关的 SOC 在数量上保持稳定,但在来源组成上并不稳定。
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引用次数: 0
Combined measurement of roots, δ18O and δ2H, and a Bayesian mixed model capture the soil profiles of wheat water uptake in a deep loamy soil 综合测量根系、δ18O 和 δ2H,并利用贝叶斯混合模型捕捉深厚壤土中小麦吸水的土壤剖面图
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-12 DOI: 10.1016/j.still.2024.106359
Runze Zhang , Jiaxing Xu , Panxin Zhang , Yan Han , Changlu Hu , Victor Sadras , Xueyun Yang , Shulan Zhang
The profile of crop water uptake from the soil depends on rainfall regime (amount, seasonality, frequency distribution of rainfall event size), soil, crop, and management. This study, with a focus on winter wheat in a wheat-fallow system, combines measurements of hydrogen (δD) and oxygen (δ18O) isotopes with a Bayesian mixing model (MixSIAR), and measurements of root length density to (i) quantify crop water uptake from soil down to 3 m depth, (ii) to assess the influence of soil water at sowing, soil mulching, seasonal conditions and their interaction on the profiles of soil water uptake, and (iii) to probe for relations between yield and the profiles of soil water uptake. Across treatments and seasons, water uptake at jointing featured a ratio 2.1: 1.0: 1.8: 2.2 in four soil layers, top 0.2 m, 0.20.4 m, 0.41.2 m, and 1.2–3.0 m. At anthesis, the ratios shifted to 5.2: 1.0: 1.7: 2.0. Water uptake at jointing was higher from top-soil in dry (∼60 %) than in wet condition (∼30 %), and the opposite was true in deeper layers; water supply had a smaller effect on the profiles of water uptake at anthesis. Compared to bare ground, mulch favored root proliferation and water uptake in 0.42.0 m soil layer. For a given soil layer, soil moisture correlated negatively with root length density. Yield correlated positively and linearly with water uptake from 0.43.0 m soil at jointing, indicating that faster root development at early stages favors water uptake from deep soil in the critical period of grain yield formation. We discuss the implications of our findings for agronomic management and breeding.
作物从土壤中吸收水分的情况取决于降雨机制(降雨量、季节性、降雨事件大小的频率分布)、土壤、作物和管理。本研究以小麦-沼泽地系统中的冬小麦为重点,将氢(δD)和氧(δ18O)同位素测量与贝叶斯混合模型(MixSIAR)以及根长密度测量相结合,(i) 量化作物从土壤中吸收的水分,直至 3 米深、(ii) 评估播种时土壤水分、土壤覆盖、季节条件及其相互作用对土壤水分吸收剖面的影响,以及 (iii) 探究产量与土壤水分吸收剖面之间的关系。在不同处理和季节中,接穗时四个土层(表层 0.2 米、0.20.4 米、0.41.2 米和 1.2-3.0 米)的吸水率比为 2.1:1.0:1.8:2.2。在花期,这一比例变为 5.2:1.0:1.7:2.0。表层土壤在干燥条件下(60%∼)比潮湿条件下(30%∼)的接合处吸水率高,深层则相反;供水对开花期吸水率的影响较小。与裸地相比,地膜有利于 0.42.0 米土层的根系增殖和吸水。在特定土层中,土壤水分与根长密度呈负相关。产量与 0.43.0 米土层接合处的吸水率呈线性正相关,表明在谷物产量形成的关键时期,早期根系的快速发展有利于从深层土壤中吸水。我们讨论了研究结果对农艺管理和育种的影响。
{"title":"Combined measurement of roots, δ18O and δ2H, and a Bayesian mixed model capture the soil profiles of wheat water uptake in a deep loamy soil","authors":"Runze Zhang ,&nbsp;Jiaxing Xu ,&nbsp;Panxin Zhang ,&nbsp;Yan Han ,&nbsp;Changlu Hu ,&nbsp;Victor Sadras ,&nbsp;Xueyun Yang ,&nbsp;Shulan Zhang","doi":"10.1016/j.still.2024.106359","DOIUrl":"10.1016/j.still.2024.106359","url":null,"abstract":"<div><div>The profile of crop water uptake from the soil depends on rainfall regime (amount, seasonality, frequency distribution of rainfall event size), soil, crop, and management. This study, with a focus on winter wheat in a wheat-fallow system, combines measurements of hydrogen (δD) and oxygen (δ<sup>18</sup>O) isotopes with a Bayesian mixing model (MixSIAR), and measurements of root length density to (i) quantify crop water uptake from soil down to 3 m depth, (ii) to assess the influence of soil water at sowing, soil mulching, seasonal conditions and their interaction on the profiles of soil water uptake, and (iii) to probe for relations between yield and the profiles of soil water uptake. Across treatments and seasons, water uptake at jointing featured a ratio 2.1: 1.0: 1.8: 2.2 in four soil layers, top 0.2 m, 0.2<img>0.4 m, 0.4<img>1.2 m, and 1.2–3.0 m. At anthesis, the ratios shifted to 5.2: 1.0: 1.7: 2.0. Water uptake at jointing was higher from top-soil in dry (∼60 %) than in wet condition (∼30 %), and the opposite was true in deeper layers; water supply had a smaller effect on the profiles of water uptake at anthesis. Compared to bare ground, mulch favored root proliferation and water uptake in 0.4<img>2.0 m soil layer. For a given soil layer, soil moisture correlated negatively with root length density. Yield correlated positively and linearly with water uptake from 0.4<img>3.0 m soil at jointing, indicating that faster root development at early stages favors water uptake from deep soil in the critical period of grain yield formation. We discuss the implications of our findings for agronomic management and breeding.</div></div>","PeriodicalId":49503,"journal":{"name":"Soil & Tillage Research","volume":"246 ","pages":"Article 106359"},"PeriodicalIF":6.1,"publicationDate":"2024-11-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142643023","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
Land degradation decreased crop productivity by altering soil quality index generated by network analysis 土地退化通过改变网络分析得出的土壤质量指数来降低作物产量
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-09 DOI: 10.1016/j.still.2024.106354
Ming Gao , Wei Hu , Xingyi Zhang , Meng Li , Yongsheng Yang , Renfeng Che
Soil erosion is a principal mechanism of land degradation, and wind erosion is particularly marked in northeast China due to its ecological characteristics. However, most investigations on the implications of land degradation on soil quality and crop productivity have concentrated on water-erosion regions, and little focus has been placed on the wind-erosion region. Therefore, we examined the impacts of land degradation on soil quality and crop productivity in the degradation area of Horqin Sandy Land, the wind-eroded region of northeast China, which suffers from varying intensities of land degradation, that is, no degraded grassland, lightly, moderately, and severely degraded croplands. In our study, network analysis (NA) was applied as a novel approach to calculate the soil quality index (SQI), which covered 11 physical, 12 chemical, and 6 biological variables measured in the 0–20 cm soil layer as indicators of soil quality. Results showed that land degradation resulted in adverse effects on soil properties. SQI, crop yield, and above-ground biomass significantly decreased with land degradation increasing (P < 0.05). Specifically, the result of NA showed soil organic carbon, microbial biomass carbon, and bulk density (BD) were the most responsive factors impacting SQI under land degradation. Structural equation modeling showed that land degradation led to the reduction of crop productivity by altering soil properties and then changing SQI. Soil physical properties were the best mediator for the indirect effects of land degradation on SQI. In addition, the BD increased, but clay, soil total nitrogen, and organic matter content decreased from 1981 to 2022, which reveals land degradation in this area. Our investigation provides a theoretical foundation for preserving cropland in wind-eroded areas of northeast China.
水土流失是土地退化的主要机制,而东北地区的生态特点决定了其风蚀尤为明显。然而,有关土地退化对土壤质量和作物生产力影响的研究大多集中在水蚀区,很少关注风蚀区。因此,我们研究了东北风蚀地区科尔沁沙地退化区的土地退化对土壤质量和作物生产力的影响,该地区存在不同程度的土地退化,即无退化草地、轻度、中度和重度退化耕地。在我们的研究中,网络分析(NA)作为一种新方法被用于计算土壤质量指数(SQI),该指数涵盖了在 0-20 厘米土层中测量的 11 个物理变量、12 个化学变量和 6 个生物变量,作为土壤质量的指标。结果表明,土地退化对土壤性质产生了不利影响。随着土地退化程度的增加,SQI、作物产量和地上生物量显著下降(P < 0.05)。具体而言,NA 结果显示,土壤有机碳、微生物生物量碳和容重(BD)是土地退化条件下影响 SQI 的最敏感因子。结构方程模型显示,土地退化通过改变土壤特性进而改变 SQI,导致作物生产力下降。土壤物理特性是土地退化对 SQI 间接影响的最佳中介。此外,从 1981 年到 2022 年,BD 增加了,但粘土、土壤全氮和有机质含量却减少了,这揭示了该地区的土地退化。我们的研究为保护东北风蚀地区的耕地提供了理论依据。
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引用次数: 0
Modeling compaction effects on hydraulic properties of soils using limited information 利用有限信息模拟压实对土壤水力特性的影响
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-06 DOI: 10.1016/j.still.2024.106349
Andre Peters , Kai Germer , Mahyar Naseri , Lennart Rolfes , Marco Lorenz
Soil compaction leads to an increase in bulk density (ρb) and a shift in the pore-size distribution towards smaller pores. This in turn changes the soil hydraulic properties (SHP), i.e., the water retention curve (WRC) and the hydraulic conductivity curve (HCC). Up to now, attempts to model the effect of altered ρb on SHP has been limited to SHP models that account only for capillary water, neglecting water stored and transmitted in adsorbed films (non-capillary water). We combine a recently developed model for compaction effects on SHP with a SHP model system, which accounts for both capillary and non-capillary water (Peters-Durner-Iden model system - PDI). Due to a plausible course of the PDI-WRC towards oven dryness and a physically based prediction scheme of the PDI-HCC based on the WRC, the new combined approach can fully predict both soil hydraulic functions of compacted soils, even with limited information. The new approach is analyzed via a sensitivity analysis and tested with a large dataset from a silty arable soil. A comparison with an established prediction approach showed that our new approach has slightly better predictive performance within the measurement range and a more plausible course in the dry range. For our field data, the new approach performed best when only 2 of the water retention parameters were scaled based on the known ρb. One of them determines the adsorptive water content and the other the shift of the capillary retention function on suction axis. Both parameters can be considered model independent, indicating that the new approach may not need calibration for each capillary retention model within the PDI model system.
土壤压实会导致容重(ρb)增加,孔隙大小分布向更小的孔隙移动。这反过来又会改变土壤的水力特性(SHP),即保水曲线(WRC)和导水曲线(HCC)。迄今为止,对改变的 ρb 对 SHP 的影响进行建模的尝试仅限于只考虑毛细管水的 SHP 模型,而忽略了吸附膜中储存和传输的水(非毛细管水)。我们将最近开发的 SHP 压实效应模型与同时考虑毛细管水和非毛细管水的 SHP 模型系统(Peters-Durner-Iden 模型系统 - PDI)相结合。由于 PDI-WRC 走向烘箱干燥的过程是可信的,并且 PDI-HCC 是基于 WRC 的物理预测方案,因此即使信息有限,新的组合方法也能完全预测压实土壤的两种土壤水力功能。通过敏感性分析对新方法进行了分析,并使用淤泥质耕地土壤的大型数据集进行了测试。与已有的预测方法进行比较后发现,我们的新方法在测量范围内的预测性能略好,而在干燥范围内的预测结果更可信。对于我们的实地数据,当只有两个保水参数根据已知的 ρb 进行缩放时,新方法的性能最佳。其中一个是吸附水含量,另一个是吸力轴上毛细滞留函数的移动。这两个参数可视为与模型无关,这表明新方法可能不需要对 PDI 模型系统中的每个毛细管滞留模型进行校准。
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引用次数: 0
Network analysis was effective in establishing the soil quality index and differentiated among changes in land-use type 网络分析可有效确定土壤质量指数,并区分土地利用类型的变化
IF 6.1 1区 农林科学 Q1 SOIL SCIENCE Pub Date : 2024-11-05 DOI: 10.1016/j.still.2024.106352
Ming Gao , Wei Hu , Meng Li , Shuli Wang , Lin Chu
Understanding the implications of land-use type on soil quality and function is critical to the adoption of suitable agricultural management practices in a specific region. Principal component analysis (PCA) is a widespread technique for calculating soil quality index (SQI), but it cannot correctly evaluate soil quality in some cases. Network analysis (NA) is a novel and effective technique for calculating SQI for determining susceptibility in different land uses but it is still limited. Moreover, few studies have compared NA and PCA to quantify soil quality. This study aimed to develop valid and accurate SQIs through NA and PCA to estimate the impacts of land-use types (cropland, forest, and grassland) on SQIs in Tongliao and Qiqihar, which are the two regions subject to frequent wind erosion in northeast China. A total of 27 soil physical, chemical, and biological properties were measured for the selection of the minimum data set (MDS), and eight SQI values were determined for each study site using additive or weighted methods and linear or nonlinear scoring functions. Results indicated that most soil attributes and SQIs varied markedly among three land-use types and were greater in grasslands or forests than in croplands. The amount of MDS generated using NA was considerably low, but soil physicochemical and biological properties were comprehensively covered. SOC in Tongliao and SHC in Qiqihar were selected by both methods and were considered the most sensitive soil quality indicators for detecting the effects of land-use types. The soil sensitivity index of the SQI calculated by NA (1.34–2.02) was higher than that of the SQI calculated by PCA (1.30–1.80). Thus, NA was more effective than PCA in computing the SQI and differentiated among changes in land use better as a simple and stable tool. The SQI developed through NA using the weighted method and nonlinear scoring function is a suitable and practical quantitative tool for SQI assessment, which is proposed to be used for soil quality assessment for various land-use types in northeast China.
了解土地利用类型对土壤质量和功能的影响对于在特定地区采用合适的农业管理方法至关重要。主成分分析法(PCA)是计算土壤质量指数(SQI)的一种常用技术,但在某些情况下并不能正确评估土壤质量。网络分析(NA)是计算 SQI 的一种新颖而有效的技术,可用于确定不同土地用途的易感性,但其应用范围仍然有限。此外,很少有研究对 NA 和 PCA 在量化土壤质量方面进行比较。本研究旨在通过 NA 和 PCA 建立有效、准确的 SQIs,以估算东北地区风蚀频发的通辽和齐齐哈尔两地的土地利用类型(耕地、森林和草地)对 SQIs 的影响。为选择最小数据集(MDS),共测量了 27 种土壤物理、化学和生物属性,并使用加法或加权法以及线性或非线性评分函数确定了每个研究地点的 8 个 SQI 值。结果表明,大多数土壤属性和 SQIs 在三种土地利用类型之间存在明显差异,草地或森林中的差异大于耕地中的差异。使用 NA 生成的 MDS 数量较少,但全面涵盖了土壤理化和生物属性。两种方法都选择了通辽的 SOC 和齐齐哈尔的 SHC,它们被认为是检测土地利用类型影响的最灵敏的土壤质量指标。NA 计算的 SQI 土壤敏感性指数(1.34-2.02)高于 PCA 计算的 SQI 土壤敏感性指数(1.30-1.80)。因此,作为一种简单稳定的工具,NA 在计算 SQI 方面比 PCA 更有效,也更能区分土地利用的变化。利用加权法和非线性评分函数,通过 NA 建立的 SQI 是一种适用、实用的 SQI 定量评价工具,建议用于东北地区不同土地利用类型的土壤质量评价。
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