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Topography and land use effects on the spatial variation of soil organic carbon: A case study in a typical small watershed of the black soil region in northeast China

机译:地形和土地利用对土壤有机碳空间变化的影响:以东北黑土区典型小流域为例

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Soil organic carbon is a soil property of central importance for soil quality and the global carbon cycle. Studies specifically aimed at the relationship between the spatial variation of soil organic carbon and environmental factors are few. In this paper, a typical small watershed named Tongshuang in the black soil region of northeast China, which was subjected to drastic erosion before 1980 and was managed subtly after 1980, was chosen as a study area. Classical statistic and geostatistic analysis methods, in combination with a geographic information system (GIS), were used to quantitatively research the spatial variation characteristics of the soil organic carbon and their relation to the topographic factors and land use. The data on the soil organic carbon, topographic factors, and land use were obtained by soil sampling and measurements derived from DEM, remote sensing images, and field investigations, respectively. The classical statistics analysis results indicated that the variability of the soil organic carbon was moderate (C-v = 0.30). The slope position and land use types were the most discriminating factors. The soil organic carbon content was the highest in the grassland and lowest in the coniferous forest (P < 0.01). It increased gradually along the slope position gradients from the interfluve to the toe slope. The geostatistics analysis showed that the soil organic carbon had a strong spatial correlation. The C-0/(C-0 + C) was 0.1608, which was mainly induced by structural factors. The mean soil organic content is 2.27% in this watershed. It is on a very low level in the northern black soil of northeast China. In this small watershed of the eroded black soil region, the present soil and water conservation measures play an important role in controlling the soil loss. However, the soil organic carbon's restoration is unsatisfactory. Nearly three-quarters of the land has worrisome productivity. How to improve the soil organic carbon content while targeting the soil fertility is a pressing need.
机译:土壤有机碳是对土壤质量和全球碳循环至关重要的土壤特性。专门针对土壤有机碳的空间变化与环境因素之间关系的研究很少。本文选择了一个典型的小流域作为研究区,该流域是中国东北黑土地区的一个小流域,该流域在1980年前遭受了严重侵蚀,并在1980年后得到了巧妙管理。利用经典的统计和地统计分析方法,结合地理信息系统(GIS),定量研究了土壤有机碳的空间变化特征及其与地形因子和土地利用的关系。土壤有机碳,地形因子和土地利用的数据分别通过土壤采样和测量获得,这些数据分别来自DEM,遥感图像和野外调查。经典统计分析结果表明,土壤有机碳的变异性中等(C-v = 0.30)。坡度位置和土地利用类型是最有区别的因素。土壤有机碳含量最高的是草地,最低的是针叶林(P <0.01)。它沿着坡度从坡道到脚趾的坡度逐渐增加。地统计学分析表明,土壤有机碳具有很强的空间相关性。 C-0 /(C-0 + C)为0.1608,这主要是由结构因素引起的。该流域的平均土壤有机含量为2.27%。它在中国东北的北部黑土中含量很低。在受侵蚀的黑色土壤区域的这个小流域,目前的水土保持措施在控制土壤流失方面起着重要作用。但是,土壤有机碳的恢复效果不理想。近四分之三的土地生产力令人担忧。当务之急是如何在提高土壤肥力的同时提高土壤有机碳含量。

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