首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >CO2 fluxes and drivers as affected by soil type, tillage and fertilization.
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CO2 fluxes and drivers as affected by soil type, tillage and fertilization.

机译:土壤类型,耕作和施肥对CO 2 通量和驱动因子的影响

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摘要

Importance of agricultural practices for greenhouse gases mitigation is examined worldwide. However, there is no consensus on CO2 emissions as affected by soil management practices. Deeper understanding of soil CO2 fluxes and drivers under different management practices are needed. The investigation of net CO2 exchange rate as dependent variable and drivers (soil water and temperature, air temperature) as affected by soil type (loam and sandy loam), tillage (conservation and no-tillage) and fertilization are presented. Soil management practices and weather conditions affected the CO2 flux through effects on soil water and temperature regime. Mean net CO2 exchange rate on sandy loam was 8% higher than on loam. No-tillage, as a moisture-conserving tool, could be an appropriate tool for CO2 emissions mitigation in any weather conditions on sandy loam; however, the advantage of no-tillage on loam was negligible. Mineral NPK fertilizers promoted significantly higher net CO2 exchange rate in both soils, but suppressed it by 15% on sandy loam during a normal year. Effect of soil water content on net CO2 exchange rate was direct in all tillage and fertilization treatments in both loam and sandy loam, whereas this effect was positive only in dry and normal weather conditions. In wet weather conditions, the direct effect of soil water content on net CO2 exchange rate was negative. Soil and air temperature acted indirectly on net CO2 exchange rate. The increase in temperature markedly suppressed the positive direct impact of soil water content on net CO2 exchange rate in dry weather conditions, but did not reduce the direct effect of soil water content in normal weather conditions. In a wet year the negative indirect effect of increased temperature enhanced the negative direct impact of soil water surplus on net CO2 exchange rate.
机译:在全世界范围内,研究了农业实践对减少温室气体的重要性。然而,由于土壤管理实践的影响,关于二氧化碳排放量尚未达成共识。需要对不同管理方式下的土壤二氧化碳通量和驱动因素有更深入的了解。研究了净CO2交换率作为因变量以及受土壤类型(壤土和沙壤土),耕作(保护和免耕)和施肥影响的驱动因素(土壤水和温度,气温)。土壤管理实践和天气条件通过影响土壤水分和温度状况影响了CO2通量。沙壤土的平均净CO2交换率比壤土高8%。免耕作为一种节约水分的工具,可能是在任何天气条件下减轻沙壤土二氧化碳排放量的适当工具;但是,免耕免耕的优势微不足道。矿物NPK肥料可显着提高两种土壤的净CO2交换率,但在正常年份中,在沙壤土上将其抑制了15%。在壤土和沙质壤土的所有耕作和施肥处理中,土壤含水量对净CO2交换率的影响都是直接的,而仅在干旱和正常天气条件下,这种影响才是正的。在潮湿天气条件下,土壤含水量对净CO2交换率的直接影响为负。土壤和气温间接影响净CO2交换率。温度升高明显抑制了干旱条件下土壤含水量对净CO2交换率的正向直接影响,但没有降低正常天气条件下土壤含水量的直接影响。在潮湿的一年中,温度升高的负面间接影响增强了土壤水分过剩对净CO2交换率的负面直接影响。

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