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首页> 外文期刊>Communications in Soil Science and Plant Analysis >Spatial and temporal variability of soil organic carbon in the corn belt of Northeastern China, 1980 s-2005: a case study in four counties.
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Spatial and temporal variability of soil organic carbon in the corn belt of Northeastern China, 1980 s-2005: a case study in four counties.

机译:1980 s-2005年中国东北玉米带土壤有机碳的时空变化:以四个县为例。

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摘要

Estimates of changes and possible causes of regional soil organic carbon (SOC) are critical for evaluation of potential responses of terrestrial biosphere to global changes. A total of 382 soil samples, collected in the 1980 s from four counties in the Corn Belt of northeastern China, and of 1,514 samples collected in 2005 from the same area, were examined for SOC concentrations. Spatial and temporal SOC concentrations were evaluated after the 25-year interval using geostatistics and kriging interpolation method. Results indicated that the average topsoil SOC concentrations of the study area increased from 1.24% in the 1980 s to 1.47% in 2005. Spatial distributions of SOC in the two separate evaluations showed greater SOC concentrations in the middle part of the study area and lower SOC concentrations in the remaining areas. From the 1980 s to 2005, SOC concentrations in the central part increased, whereas those in the northeastern and southwestern parts decreased. The increasing trend of SOC concentrations might be attributed to the land-use and land cover changes, crop productivity increase, and agricultural management.
机译:变化的估计和区域土壤有机碳(SOC)的可能原因对于评估陆地生物圈对全球变化的潜在响应至关重要。对1980年代从中国东北玉米带的四个县收集的382个土壤样品和2005年从同一地区收集的1,514个样品进行了SOC浓度检查。在25年的间隔后,使用地统计学和克里格插值法评估了时空SOC浓度。结果表明,研究区的平均表层土壤SOC浓度从1980年代的1.24%增加到2005年的1.47%。两次独立评估中SOC的空间分布表明,研究区中部的SOC浓度较高,而SOC较低其余区域的浓度。从1980年代到2005年,中部的SOC浓度增加,而东北部和西南部的SOC浓度下降。 SOC浓度增加的趋势可能归因于土地利用和土地覆盖的变化,作物生产力的提高以及农业管理。

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