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广西崇左市白头叶猴保护区土壤研究
引用本文:陈作雄.广西崇左市白头叶猴保护区土壤研究[J].广西师范学院学报(自然科学版),2011,28(1):58-67.
作者姓名:陈作雄
作者单位:广西师范学院,广西南宁,530001
摘    要:在现代的南亚热带高温多雨的气候作用下,赤红壤继续处于高度淋溶状态而发育成盐基高度不饱和,酸性较强,有机质量较低,土壤肥力较差;而处于岩溶山地的坡麓和谷地中的红粘土,因受山上的富含钙镁的岩溶水淀积复钙和淋溶脱钙的反复作用发育形成红色石灰土或复钙红粘土.这在广西崇左市白头叶猴保护区区的濑湍片、板利片和岜盆片的峰林谷地中和河...

关 键 词:广西  崇左市  保护区  土壤  研究

A Research into the White- headed Langur Reserve Soil of Chongzuo City
CHEN Zuo-xiong.A Research into the White- headed Langur Reserve Soil of Chongzuo City[J].Journal of Guangxi Teachers Education University:Natural Science Edition,2011,28(1):58-67.
Authors:CHEN Zuo-xiong
Institution:CHEN Zuo-xiong(Guangxi Teachers Education University,Nanning 530001,China)
Abstract:The distribution of the karst terraces and basin levels in the area of red soil known as the red clay is the product of a high-degreed weathering and leaching,conditioned for a long time by tropical and subtropical climate in the late Tertiary to Quaternary Pleistocene.In the present hot and rainy tropical climate of South Asia,under the effect of leaching of red soil in a high state to continue developing into a base of highly unsaturated,acidic,low organic content,soil fertility is poor.The red clay of the slope in karst hills and valleys,rich in calcium and magnesium,is undergoing the development of the repeated formation of decalcified limestone soil or re-calcified red clay,which is due to karst water and leaching of calcium deposition complex.This is widespread in the peaks-valleys and valley terraces of Laituan,Banli and Bapen in the white-headed langur reserve of Chongzuo,Guangxi.
Keywords:Guangxi  Chongzuo  reserve  soil  research
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