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首页> 外文期刊>Geoderma: An International Journal of Soil Science >Spatial distribution of caliche nodules in surface soil and their influencing factors in the Liudaogou catchment of the northern Loess Plateau, China
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Spatial distribution of caliche nodules in surface soil and their influencing factors in the Liudaogou catchment of the northern Loess Plateau, China

机译:中国北黄土高原Liudaogou集团中Caliche Nodules的空间分布及其影响因素

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摘要

Quantifying the distribution of caliche nodules in a catchment is a basis toward understanding soil erosion and soil degradation as well as soil-water processes in the soil containing caliche nodules. In this study, field surveys and soil sampling were coupled with spatial and statistical analyses along with image processing to investigate the spatial distribution of caliche nodules and their influencing factors in the Liudaogou catchment, the northern Loess Plateau of China. Results showed that more caliche nodules were present at the top of the mountain, mountain ridges, roadsides, edges of ravines, and other high elevation regions, as represented by comparatively higher caliche nodule coverage (CNC, 11.26-18.28%). Caliche nodules were rarely present in low elevation areas such as the terraced cropland and check dam, as represented by lower CNC ( & 2.55%). More than 65% of the total caliche nodules had a diameter of 10-50 mm. The caliche nodule coverage and diameter showed strong spatial dependence. The CNC was significantly related to the slope gradient and vegetation cover (P & 0.01), and the caliche nodule diameter (CND) was significantly related to the elevation (P & 0.01). Two simple models were established to predict the CNC and CND values given the parameters of slope gradient and vegetation cover. The validation of the models showed relatively high accuracy. These findings quantify caliche nodule distribution in a catchment for the first time, and may benefit the assessment of soil erosion and soil degradation in this special soil in the Loess Plateau.
机译:量化集水中的Caliche Nodules的分布是了解土壤侵蚀和土壤降解以及含有Caliche结节的土壤中的土壤水处理的基础。在本研究中,现场调查和土壤采样与空间和统计分析以及图像处理以及调查Caliche Nodules的空间分布及其在中国北黄土高原Liudaogou集水区中的空间分布及其影响因素。结果表明,在山顶,山脊,沟道,沟壑,沟壑的顶部以及其他高仰角区的顶部存在更多的Caliche Nodules,如相对较高的Caliche Nodule覆盖(CNC,11.26-18.28%)所代表。 Caliche Nodules很少存在于低仰角区域,例如梯田农作物和校验坝,如下CNC(& 2.55%)所示。超过65%的Caliche Nodules的直径为10-50毫米。 Caliche Nodule覆盖率和直径显示出强烈的空间依赖性。 CNC与坡度梯度和植被覆盖(P& 0.01)显着相关,并且Caliche Nodule直径(CND)与升高有关(P& 0.01)显着相关。考虑到斜坡梯度和植被覆盖的参数,建立了两个简单的模型来预测CNC和CND值。模型的验证表现出相对高的准确性。这些发现是第一次定量集水中的Caliche结节分布,并可能有利于黄土高原在黄土高原的特殊土壤中的土壤侵蚀和土壤降解评估。

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