State Key Laboratory of Resources and Environmental Information System, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China.
University of Chinese Academy of Sciences, Beijing 100049, China.
Int J Environ Res Public Health. 2018 Aug 23;15(9):1818. doi: 10.3390/ijerph15091818.
Based on soil sampling data from the dry season and the rainy season, the spatial heterogeneity and spatial pattern of soil nutrients in the Mun River Basin, Thailand, were studied and the seasonal variation in soil nutrients was analyzed using classical statistical methods and geostatistical methods. The soil nutrient content in the Mun Basin showed moderate and strong variations, and the descending order of soil variability was as follows: available phosphorous (AP) > electric conductivity (EC) > soil organic matter (SOM) > total nitrogen (TN) > pH value in the dry season, with AP showing strong variation, and EC > AP > SOM > TN > pH in the rainy season, with EC showing strong variation. Different soil nutrients and different soil properties had different spatial variation characteristics, and their corresponding best-fitting models were also different. Based on the nugget (C₀), sill (C₀ + C), and range (A), spatial analysis was performed for the soil nutrients, pH, and EC in the dry season and in the rainy season. Analysis based on kriging spatial interpolation data showed that pH, SOM, TN, and EC had convex or concave distributions, whereas AP had a patchy distribution. Terrain, vegetation, and human disturbance are the main factors that contribute to the differences in the soil nutrient pattern of the Mun River Basin.
基于旱季和雨季的土壤采样数据,研究了泰国漫河盆地土壤养分的空间异质性和空间格局,并采用经典统计方法和地统计学方法分析了土壤养分的季节性变化。漫河流域土壤养分含量具有中等和较强的变异性,土壤变异性的降序为:有效磷(AP)>电导率(EC)>土壤有机质(SOM)>全氮(TN)>旱季 pH 值,其中 AP 表现出较强的变异性,EC>AP>SOM>TN>雨季 pH 值,其中 EC 表现出较强的变异性。不同的土壤养分和不同的土壤性质具有不同的空间变异特征,其相应的最佳拟合模型也不同。基于块金值(C₀)、基台值(C₀+C)和范围值(A),对旱季和雨季的土壤养分、pH 值和 EC 进行了空间分析。基于克立格空间插值数据的分析表明,pH 值、SOM、TN 和 EC 具有凸或凹的分布,而 AP 具有斑块状分布。地形、植被和人为干扰是导致漫河流域土壤养分格局差异的主要因素。