广南县幅岩溶区与非岩溶区土壤碳氮磷生态化学计量比空间变异分析

借助1∶25万云南省广南县幅土壤地球化学调查数据，并利用单因素方差分析、多重比较法以及地统计学方法，对岩溶区和非岩溶区土壤碳氮磷生态化学计量特征及其空间分布进行了对比分析。结果显示:广南县幅岩溶区土壤中有机碳（SOC）、全氮（TN）、全磷（TP）含量显著高于非岩溶区，而碳氮比（C∶N）、碳磷比（C∶P）、氮磷比（N∶P）显著低于非岩溶区；无论是岩溶区还是非岩溶区，表层（0～20 cm）SOC、TN、C∶N、C∶P、N∶P均显著高于深层（＞100 cm）。克里格空间插值结果表明，研究区表层土壤中SOC、TN、TP含量具有东高西低的特征，而C∶N、C∶P、N∶P具有低值区集中于东部、高值区散布在西部的空间分布格局。成土母质和土壤类型等自然因素严重制约了研究区土壤碳氮磷的空间变异，同时土地利用变化等人为因素也起到了不可忽视的作用。 

Spatial variation analysis of soil carbon, nitrogen and phosphorus eco-stoichiometric ratios in karst and non-karst areas of Guangnan county, Yunnan, China

The ratio of soil carbon, nitrogen and phosphorus is an important indicator of soil organic matter composition and quality. However, soil has a high degree of spatial heterogeneity. In karst areas, the composition of soil geochemical elements is special, the ecological environment is vulnerable, and the natural environment is vignificantly different from non-karst areas. Therefore, it is necessary to understand spatial and temporal distributions and the migration mechanism of essential elements, such as carbon, nitrogen and phosphorus, for vegetation growth in the soils of both karst areas and non-karst areas. The study area of current study is located in Guangnan county, Yunnan Province, where karst areas account for 197.52 km2 and non-karst areas for 205.39 km2. The soil composition data for 102 surface composite soil samples and 24 deep composite soil samples were obtained from the soil geochemical survey on the scale of 1∶250,000. In this paper, one-way ANOVA, multiple comparison analysis and geostatistical method were utilized to compare the characteristics of soil carbon, nitrogen and phosphorus eco-stoichiometry and spatial variability between karst areas and non-karst areas, so as to explore the possible factors leading to this spatial variability and provide a reliable basis for ecological environment management and soil remediation. The results showed that in general, the contents of soil organic carbon(SOC), total nitrogen(TN) and total phosphorus(TP) in the karst area were significantly higher than those in the non-karst area, while the carbon to nitrogen ratio(C∶N) , carbon to phosphorus ratio(C∶P) and nitrogen to phosphorus ratio(N∶P) were significantly lower than non-karst area. Whether in karst areas or in non-karst areas, the content of SOC, TN and the C∶N, C∶P, N∶P ratio in the surface soil (0-20 cm) were significantly higher than those in the deep soil (>100 cm). Kriging interpolation results indicated that the contents of SOC, TN, TP in the surface soil were characterized by low in west and high in east of the study area; while the C∶N, C∶P, N∶P had a spatial distribution pattern of low values concentrated in the east and high values scattered in the west. In addition, there were differences in nutrient contents among different soil types, with the highest content of SOC, TN and TP in yellow-purple-mud soil and the lowest content of them in acid yellow-red soil. Natural factors, such as pedogenic parent rocks and soil types, have seriously controlled spatial variation of the soil carbon, nitrogen and phosphorus. Meanwhile, anthropic factors, such as land use change, also play an important role, which can not be ignored.