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Conservation management improves agroecosystem function and resilience of soil nitrogen cycling in response to seasonal changes in climate

机译:保护管理改善了农业系统功能和土壤氮循环的恢复力,以应对气候季节变化

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摘要

Understanding how conservation agricultural management improves soil nitrogen (N) stability in the face of climate change can help increase agroecosystem productivity and mitigate runoff, leaching and downstream water quality issues. We conducted a 2-year field study in a 36-year-old rain-fed cotton production system to evaluate the impacts of changing climatic factors (temperature and precipitation) on soil N under conservation management, including moderate inorganic N fertilizer application (0 and 67 kg N ha~(-1)), winter cover crops (fallow; winter wheat, Triticum aestivum L.; hairy vetch, Vicia villosa Roth), and reduced tillage (no-till; disk tillage). Structural equation modeling (SEM) was used to quantify and compare the effects of conservation management and climatic factors on soil N concentrations. Fertilizer and vetch cover crops increased soil total N concentration by 16% and 18%, respectively, and also increased microbial N transformation rate by 41 % and 168%. In addition, vetch cover crops also increased soil labile N concentrations by 57%, 21%, and 79%, i.e., extractable organic N, ammonium, and nitrate, respectively. The highest soil δ~(15)N value (6.4 ± 0.3‰) was observed under the 67 kg N ha~(-1) fertilizer-wheat-disk tillage treatment, and the lowest value (4.8 ± 0.3‰) under the zero-fertilizer-wheat-no-till treatment, indicating fertilizer and tillage might accelerate microbial N transformation. The SEM showed positive effects of temperature and precipitation on labile N concentrations, suggesting destabilization of soil N and the potential for soil N loss under increased temperature and intensified precipitation. Fertilizer and vetch use might mitigate some of the effects of temperature by accelerating microbial N transformations, with vetch having a larger effect than fertilizer (0.35 vs. 0.15, Table 1). No-till can reduce some of the effects of precipitation on soil labile N by maintaining soil structure. Our study suggests that fertilizer, vetch cover crop, and no-till might help improve function and resilience of agroecosystems in relation to soil N cycling. Soil N stabilization in cropping systems can be enhanced by adjusting agricultural management.
机译:了解保护农业管理如何改善土壤氮气(N)稳定性,面对气候变化,有助于提高农业体系生产力和缓解径流,浸出和下游水质问题。我们在一家36岁的雨水棉花生产系统中进行了2年的实地研究,以评估缓解管理中变化的气候因子(温度和降水)的影响,包括中等无机N肥料应用(0和67千克HA〜(-1)),冬季覆盖作物(休耕;冬小麦,Triticum Aestivum L.毛茸茸的朱迪,维尼亚villosa罗斯),减少耕作(无直到;磁盘耕作)。结构方程建模(SEM)用于量化和比较保护管理和气候因子对土壤浓度的影响。肥料和拔胶覆盖作物分别将土壤总浓度增加16%和18%,也增加了微生物N转化率高41%和168%。此外,读取覆盖作物还将土壤不稳定浓度增加57%,21%和79%,即可提取的有机氮和硝酸铵。在67kg N Ha〜(-1)肥料 - 小麦盘耕作处理下观察到最高土壤δ〜(15)n值(6.4±0.3‰),零下的最低值(4.8±0.3‰) - 小麦 - 小麦无直到治疗,表明肥料和耕作可能会加速微生物N转化。 SEM显示出温度和沉淀对不稳定N浓度的阳性作用,表明土壤N的稳定化以及在提高温度下降沉的土壤损失的潜力。肥料和vetch使用可以通过加速微生物N转化来减轻一些温度的影响,蒸煮具有比肥料更大的效果(0.35 vs.015,表1)。通过维持土壤结构,无直到可以减少沉淀对土壤不稳定N的一些影响。我们的研究表明,肥料,虫胶覆盖作物和禁止,可能有助于提高农业体系与土壤循环的函数和恢复性。通过调整农业管理,可以提高种植系统中的土壤n稳定。

著录项

  • 来源
    《Science of the total environment》 |2021年第20期|146457.1-146457.11|共11页
  • 作者单位

    University of Tennessee-Knoxville Department of Biosystems Engineering and Soil Science 2506 E.J. Chapman Drive Knoxville TN 37996 USA USDA-ARS Agroecosystem Management Research Unit 251 Filley Hall UNL-East Campus Lincoln NE 68583 USA;

    University of Tennessee-Knoxville Department of Biosystems Engineering and Soil Science 2506 E.J. Chapman Drive Knoxville TN 37996 USA Blount County Soil Conservation District 1217 McArthur Rd Maryville TN 37804 USA;

    USDA-ARS Agroecosystem Management Research Unit 251 Filley Hall UNL-East Campus Lincoln NE 68583 USA;

    University of Tennessee-Knoxville Department of Biosystems Engineering and Soil Science 2506 E.J. Chapman Drive Knoxville TN 37996 USA;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Increased temperature; Intensified precipitation; Soil microbial biomass nitrogen; Soil nitrate; Soil nitrogen mineralization; Soil δ~(15)N;

    机译:温度增加;加强沉淀;土壤微生物化学生物质氮;土壤硝酸盐;土壤氮矿化;土壤δ〜(15)n;

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