首页> 外文期刊>Soil & Tillage Research >How do biodegradable organic residues affect soil CO2 emissions? Case study of a Mediterranean agro-ecosystem
【24h】

How do biodegradable organic residues affect soil CO2 emissions? Case study of a Mediterranean agro-ecosystem

机译:可生物降解的有机残留情况如何影响土壤二氧化碳排放量? 地中海农业生态系统的案例研究

获取原文
获取原文并翻译 | 示例
           

摘要

Soil respiration is the main carbon flux in the second largest terrestrial carbon pool, soil environment. Emissions of CO2 from soils are five times higher than from anthropogenic emissions (USDOE, 2008). Despite increasing atmospheric CO2 concentrations, the dynamics and driving forces for soil CO2 emissions are not well understood. This work investigates the evolution of soil respiration (Rs) in a semiarid Mediterranean agro-ecosystem after the application of three different biodegradable organic residues (BOR): municipal solid waste compost (MSWC), anaerobically (ANSS) and aerobically (AESS) digested sewage sludge. We also studied how these amendments affect the relationship between Rs and soil climate variables. The results showed a clear increase in Rs at very short time after the application, especially in AESS-treated soils. Annual evolution of Rs was highly correlated with the carbon fractions of the BORs applied, with the highest effect seen in AESS-treated soils after the application, and a moderate but more persistent effect in MSWC. ANSS showed an intermediate behaviour. The type of amendment explained 54.7% of Rs variability. The application of BOR also changed the relationship between Rs and soil climate conditions. The results showed that BOR application produced an increase in Rs positive dependence on soil temperature (Ts) and the Birch effect, and a decrease in the negative dependence on soil moisture (Ms). In untreated soils (CONT) Ts-Ms interaction was the main factor which drove Rs evolution. The results suggest using highly composted wastes (MSWC) as the best option of those analysed for medium-term carbon management in agricultural practices. (C) 2015 Elsevier B.V. All rights reserved.
机译:土壤呼吸是第二大陆地碳库,土壤环境中的主要碳通量。来自土壤的二氧化碳排放量高​​于人体排放量的五倍(USDOE,2008)。尽管大气二氧化碳浓度增加,但土壤二氧化碳排放的动力学和驱动力尚不清楚。这项工作调查了在应用三种不同的可生物降解的有机残留物(BOR)之后半干旱地中海农业生态系统中土壤呼吸(RS)的演变:城市固体废物堆肥(MSWC),厌氧(ANSS)和有氧(AESS)消化污水污泥。我们还研究了这些修正案如何影响RS和土壤气候变量之间的关系。结果表明,在施用后的短时间内,卢比的卢比显然,特别是在避难所的土壤中。 Rs的年度演化与施用的碳的碳部分高度相关,在应用后的AESS治疗土壤中看到的最高效果,以及在MSWC中的中等但更持久的效果。 ANSS显示出中间行为。修订的类型解释了54.7%的RS变异性。 Bor的应用还改变了Rs和土壤气候条件之间的关系。结果表明,BOR应用在土壤温度(TS)和桦木效应上产生了RS阳性依赖性的增加,以及对土壤水分(MS)的负依赖性的降低。在未处理的土壤(续)TS-MS相互作用中是驱动RS进化的主要因素。结果表明,使用高堆肥废物(MSWC)作为分析农业实践中期碳管理的最佳选择。 (c)2015 Elsevier B.v.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号