摘要
白鳝泥是四川盆地尤其西部广泛分布的一类耕地土壤,以田为主。白鳝泥是其基本形成过程,实质是铁、锰的还原性淋溶。由古富铝风化壳形成之白鳝泥,一般质地粘重,持水力强,铁、锰淋失量大,白鳝泥层厚。湿害和供肥能力低是其突出的生产问题。
Arable bleached soils are widely distributed in Sichuan basin, especialy in western part。Most of them are paddy soils. Bleaching is their basic process of formation. The key crux is the reductive bleaching of iron and manganese。The properties of the bleached soil formed from paleo—allitic weathering crus are heavy texture, thick albic horizon, strong water—holding powerand bleaching of iron and manganese。The obvious problems of the soil are wet and low ability of nutrient supply。
出处
《四川农业大学学报》
CSCD
1990年第4期284-297,共14页
Journal of Sichuan Agricultural University