向 娇, 宋 超, 石迎春, 董秋瑶, 杨振京. 安徽省六安地区土壤pH空间变异特征及其影响因素[J]. 土壤通报, 2021, 52(1): 34 − 41. DOI: 10.19336/j.cnki.trtb.2019103001
引用本文: 向 娇, 宋 超, 石迎春, 董秋瑶, 杨振京. 安徽省六安地区土壤pH空间变异特征及其影响因素[J]. 土壤通报, 2021, 52(1): 34 − 41. DOI: 10.19336/j.cnki.trtb.2019103001
XIANG Jiao, SONG Chao, SHI Ying-chun, DONG Qiu-yao, YANG Zhen-jing. Spatial Variation Characteristics and Influencing Factors of Soil pH in the Lu’an Area of Anhui Province[J]. Chinese Journal of Soil Science, 2021, 52(1): 34 − 41. DOI: 10.19336/j.cnki.trtb.2019103001
Citation: XIANG Jiao, SONG Chao, SHI Ying-chun, DONG Qiu-yao, YANG Zhen-jing. Spatial Variation Characteristics and Influencing Factors of Soil pH in the Lu’an Area of Anhui Province[J]. Chinese Journal of Soil Science, 2021, 52(1): 34 − 41. DOI: 10.19336/j.cnki.trtb.2019103001

安徽省六安地区土壤pH空间变异特征及其影响因素

Spatial Variation Characteristics and Influencing Factors of Soil pH in the Lu’an Area of Anhui Province

  • 摘要: 本文对安徽省六安-霍山地区土地质量地球化学调查项目取得的1295个土壤表层样品(0 ~ 20 cm)的pH值进行了统计分析,深入探讨了其空间变异特征及其影响因素。结果表明,研究区表层(0 ~ 20 cm)土壤pH变化幅度为3.97 ~ 8.09,平均值为5.38。90.57%的土壤样品pH值在研究区5.0 ~ 6.5范围内,呈酸性,局部地区土壤的pH值在5.0以下,呈强酸性;少量土壤样品呈中碱性(7.5 ~ 8.5),研究区土壤pH值整体呈现北高南低的分布特征。全区表层土壤pH呈正态分布,变异系数为7%,属于弱空间变异性。地统计学分析结果表明,研究区表层(0 ~ 20 cm)土壤pH的变异函数的最优理论模型为指数模型,块金效应值为0.387,表明受到人为因素和结构性因素的共同影响,土壤pH值具有中等程度的空间相关性。相关分析表明,研究区土壤pH值空间变异的主要控制因素为土壤类型、成土母质、地貌类型和土地利用方式,分别能独立解释研究区19.1%、11.1%、9.3%和2.5%的土壤pH值空间变异。此外,CaO、P、K2O、S元素含量与土壤pH呈弱负相关。因此,土壤类型和成土母质是安徽省六安-霍山地区土壤酸化最主要的影响因素。

     

    Abstract: The pH values of 1295 soil surface samples (0-20 cm) obtained from the project of Geochemical Survey on Soil Quality at the Lu’an-Huoshan region of Anhui Province were statistically analyzed in this study, and their spatial variability characteristics and influencing factors were discussed. The results showed that the pH of surface soil (0-20 cm) in the study area varied from 3.97 to 8.09, with an average value of 5.38. The soil samples of pH values within the range of 5.0 to 6.5 were about 90.57%, with acidic. The soil pH value in some areas was below 5.0, with strongly acidic. A small number of soil samples were moderately alkaline (7.5 to 8.5). As a whole, the distribution characteristics of pH value were higher in the north and lower in the south. The pH of surface soil in the whole region was normally distributed with a coefficient of variation of 7%, which belonged to the weak spatial variability. Geostatistical analysis results showed that the optimal theoretical model for the variation function of soil pH in the surface layer (0-20 cm) was an exponential model, and the nugget effect value was 0.423, indicating that it was affected by both human and structural factors and had a medium degree of spatial correlation. The variance analysis and regression analysis showed that the main controlling factors of spatial variability of soil pH in the study area were soil type, soil parent material, landform type, and land use pattern, which independently explained 19.1%, 11.1%, 9.3% and 2.5% of spatial variability of soil pH, respectively. In addition, the content of CaO, P, K2O and S was negatively correlated with soil pH. Therefore, soil type and soil parent material were the main factors affecting Soil acidification in the Lu’an-Huoshan area of Anhui Province.

     

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