珠海市耕地土壤有效铜含量及其影响因素研究

Dafang Wu, Yanyan Liu, Yihua Liu, Yuxiang Dong, Jianfei Chen, Y. Feng, Jianhui Du
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引用次数: 3

摘要

选择珠江三角洲的珠海市作为研究区域。土壤样品根据第二次全国土壤调查的采样点重新采集。利用地理信息系统(GIS)和SPSS软件,分析了耕地土壤中有效铜的含量、分布及其影响因素。结果表明:珠海市0 ~ 40cm耕地土壤深度有效铜含量平均为3.13mg·kg-1,变化范围为0.02 ~ 99.96mg·kg-1。随着耕地土壤深度的增加,有效铜含量范围迅速下降。不同土地利用类型的含量极差、平均值、标准差、方差、偏度和峰值由大到小依次为菜地>水田>旱地。利用线性方程、幂函数和指数函数对有效铜含量与影响因素进行回归分析,结果表明:在某些深度,pH值与有效铜含量呈正相关。有效铜含量与有机质呈显著正相关。有效铜含量与粘土含量也呈显著正相关。土壤深度为12 ~ 27cm时,pH值与有效铜含量的直线方程相关系数最大。在27 ~ 40cm土层深度,黏土含量与有效铜含量的指数函数相关系数最大。在其他土层深度,有效铜含量与其影响因素的幂函数相关系数最大。不同深度耕地有效铜含量的自然影响因子存在显著差异。pH≥Ü 7.0和pH≥3.4 7.0时,0 ~ 12cm土壤有效铜含量的影响因素依次为有机质> pH >粘土含量和粘土含量>有机质> pH; 12 ~ 27cm ~ 27 ~ 40cm土壤有效铜含量的影响因素依次为粘土含量>有机质> pH和有机质>粘土含量> pH。
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Study on Available Copper Content in Cultivated Soils and Its Affecting Factors in Zhuhai
The Zhuhai city in Pearl River Delta was chosen as a study area. The soil samples were recollected according to the sampling points of Second National Soil Survey. Based on application of geographical information system (GIS) and SPSS software, the content, distribution and its influence factors of available Cu in cultivated soils were analyzed. The results showed that: the average available copper content in soil depth of 0-40cm of cultivated land in Zhuhai is 3.13mg¡¤kg-1, variation range is 0.02-99.96mg¡¤kg-1. When the soil depth of cultivated land increased, available copper content ranges rapid decreased. The rank of content range, average, standard deviation, variance, skewness and peakness of different land use types in decreasing order is vegetable soil > paddy field > dry land. Regression analysis using line equation, power function and exponential function between available copper content and affecting factors shows that: a positive correlation exits between pH and the available copper content in some soil depth. There is a remarkable positive correlation exit between the available copper content and organic matte. The available copper content and clay content also has a remarkable positive correlation. In soil depth of 12-27cm, the correlation coefficient of line equitation between pH and the available copper content is the biggest. In soil depth of 27-40cm, the correlation coefficient of exponential function between clay content and the available copper content is the biggest. In other soil depth, the correlation coefficient of power function between the available copper content and its affecting factors are the biggest. There are significant differences among nature affecting factors of available copper content in different depth of cultivated land. When pH ¡Ü 7.0 and pH £¾ 7.0, affecting factors of available copper content in soil depth of 0-12cm in decreasing order is organic matter > pH > clay content and clay content > organic matter > pH, while affecting factors of available copper content in soil depth of 12-27cm¡¢27-40 cm in decreasing order is clay content > organic matter > pH and organic matter > clay content > pH.
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