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Responses of soil respiration to soil management changes in an agropastoral ecotone in Inner Mongolia China

机译:内蒙古农牧交错带土壤呼吸对土壤管理变化的响应

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摘要

Studying the responses of soil respiration (R s) to soil management changes is critical for enhancing our understanding of the global carbon cycle and has practical implications for grassland management. Therefore, the objectives of this study were (1) quantify daily and seasonal patterns of R s, (2) evaluate the influence of abiotic factors on R s, and (3) detect the effects of soil management changes on R s. We hypothesized that (1) most of daily and seasonal variation in R s could be explained by soil temperature (T s) and soil water content (S w), (2) soil management changes could significantly affect R s, and (3) soil management changes affected R s via the significant change in abiotic and biotic factors. In situ R s values were monitored in an agropastoral ecotone in Inner Mongolia, China, during the growing seasons in 2009 (August to October) and 2010 (May to October). The soil management changes sequences included free grazing grassland (FG), cropland (CL), grazing enclosure grassland (GE), and abandoned cultivated grassland (AC). During the growing season in 2010, cumulative R s for FG, CL, GE, and AC averaged 265.97, 344.74, 236.70, and 226.42 gC m−2 year−1, respectively. The T s and S w significantly influenced R s and explained 66%–86% of the variability in daily R s. Monthly mean temperature and precipitation explained 78%–96% of the variability in monthly R s. The results clearly showed that Rs was increased by 29% with the conversion of FG to CL and decreased by 35% and 11% with the conversion of CL to AC and FG to GE. The factors impacting the change in Rs under different soil management changes sequences varied. Our results confirm the tested hypotheses. The increase in Q10 and litter biomass induced by conversion of FG to style="fixed-case">GE could lead to increased Rs if the climate warming. We suggest that after proper natural restoration period, grasslands should be utilized properly to decrease Rs.
机译:研究土壤呼吸对土壤管理变化的响应对于增进我们对全球碳循环的理解至关重要,并且对草地管理具有实际意义。因此,本研究的目标是(1)量化Rs的每日和季节性模式;(2)评估非生物因素对Rs的影响;(3)检测土壤管理变化对Rs的影响。我们假设(1)R s的大部分每日和季节性变化都可以通过土壤温度(T s)和土壤水分(S w)来解释,(2)土壤管理变化可能会显着影响R s,以及(3)通过非生物和生物因子的显着变化,土壤管理改变了影响R s。在2009年(8月至10月)和2010年(5月至10月)的生长季节,在中国内蒙古的农牧交错带监测了原位R s值。土壤管理变化顺序包括自由放牧草地(FG),农田(CL),放牧围栏草地(GE)和废弃耕地草地(AC)。在2010年的生长季节中,FG,CL,GE和AC的累积R s平均为265.97、344.74、236.70和226.42 gC·m −2 year -1 ,分别。 T s和S w显着影响R s,并解释了每日R s的66%–86%的变异性。月平均温度和降水解释了每月R s变化的78%–96%。结果清楚地表明 R 随着FG向CL的转化, s 分别增加了29%,而CL向AC和FG向GE的转化, s 分别降低了35%和11%。影响 R 变化的因素 s 在不同土壤管理下的变化顺序不同。我们的结果证实了检验的假设。 Q 的增加FG转化为 style =“ fixed-case”> GE 诱导的 1 0 和凋落物生物量可能导致 R 升高 s (如果气候变暖)。我们建议在适当的自然恢复期后,应合理利用草地以减少 R s

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