成土母质和种植制度对土壤pH和交换性铝的影响

研究了我国南方 3种不同成土母质发育的酸性自然土壤的 p H与交换性铝含量状况和种植不同作物后它们的变化。研究结果表明 ,自然土壤的 p H平均值大小顺序为雷州半岛地区玄武岩发育砖红壤≤粤中花岗岩发育赤红壤 <粤北石灰岩发育红壤 ,土壤交换性铝含量的平均值的大小顺序为粤北石灰岩发育红壤 <雷州半岛地区玄武岩发育砖红壤 <粤中花岗岩发育赤红壤。种植茶树将使这 3种土壤的 p H显著降低 ,交换性铝的含量则将不同程度升高 ,最为明显的是种茶后石灰岩发育的茶园土的 p H在这 3种土壤中变为最低 ,交换性铝数量的增加幅度最大。种植水稻将提高土壤的 p H和交换性铝的含量。轮作花生后土壤的 p H也将上升 ,但受施用石灰的影响土壤交换性铝的含量将降低

pH and the exchangeable aluminum content in acid soils as affected by parent materials and cropping systems

As a result of high annual average temperature and plentiful rainfall, acidity of soils in south China was intensive and a large number of exchangeable aluminum (Al) was accumulated in the soils. Impacts of exchangeable Al on soil properties, soil fertility, and Al toxicity to living organisms have received ample attention. Limestone fertilization has long been regarded as an effective measure to alleviate the toxicity of soluble Al to crops planted in acid soils. Acquirement of the status of pH as well as ...