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溪源江流域土地利用方式对土壤理化性质影响

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本文以溪源江流域为例,通过单因素方差分析、Welch方差分析及Spearman相关系数,对3种土地利用方式下0~30cm土层土壤机械组成、pH值及土壤有机质(OM)间的对比及其关系进行研究。结果表明:①pH值、土壤有机质及机械组成的正态性检验峰度绝对值小于10、偏度绝对值小于3,为正态分布;所有样本数据方差齐性检验P值均小于0。05;②果园和草地、林地和草地的pH值存在显著性差异;③园地和林地的pH均值均小于7,草地pH均值大于7;有机质含量均值为林地>园地>草地;物理性黏粒含量均值为园地>林地>草地;④pH与物理性黏粒含量呈显著的负相关,与物理性砂粒含量呈显著的正相关,而OM与pH、OM与物理性黏粒含量均无相关性。
Impact of Land Use Patterns on Soil Physicochemical Properties in the Xiyuan River Watershed
The Xiyuan River Watershed was taken as the example for the comparison and study of the relations among the soil mechanical composition,pH value and soil organic matter(OM)in the 0-30 cm soil layers under three different land use patterns by using the one-way ANOVA,Welch's ANOVA,and Spearman rank correlation coefficient.The results showed that:(1)the normality test of pH value,soil organic matter,and mechanical composition indicated a normal distribution,with the absolute value of kurtosis less than 10 and absolute value of skewness less than 3.Additionally,the P-value obtained from the tests of homogeneity of variance for all sample data was less than 0.05;(2)there was a significant difference in pH value observed between the orchard and the grassland,as well as between the forest land and the grassland;(3)the mean pH value in the orchard and the forest land were both lower than 7,while mean pH value in the grassland was higher than 7.The mean values of organic matter content showed the order of forest land>orchard>grassland,while the mean values of physical clay content showed the order of orchard>forest land>grassland;(4)the significant negative correlation was found between pH and physical clay content,while the significant positive correlation was found between pH and physical sand content.However,no correlation was observed between organic matter(OM)and pH or between organic matter(OM)and physical clay content.

soil physicochemical propertiesland useANOVAXiyuan River Watershed

陈鹭、黄紫欣

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福建师范大学地理科学学院、碳中和未来技术学院,福建 福州 350108

土壤理化性质 土地利用 方差分析 溪源江流域

2024

亚热带水土保持
福建省水土保持委员会 福建省水土保持学会

亚热带水土保持

影响因子:0.38
ISSN:1002-2651
年,卷(期):2024.36(1)
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