| [1] |
(1)熊毅，1944，江西更新统枯土之性质及其生成，地质论评，9卷1-2期，109-1200 (2)熊毅，1952,由更新统沉积物的胶体矿物分析试论第四纪气候，地质学报，32卷,26-410 (3)Alexiades, C. A, and Jackson, M, I.，1966: Quantitative clay mineralogical analysis of soils and sediments, Clays Clay Miner. 14, 35-52 (4)Jackson, M, L,，1964: Soil clay mineralogical analysis in C, L. Rich and G, W, Kunze(eds)。Soil Clay Mineralogy, p.245-294, The University of North Carolona Press Chapel Hill, (5)Herrera, R. Garcia, Miragaya, J, and Mayorga, O, 1980e Effect. of the removal of free iron oxides 0n the cation exchange capacity at various pH"s and surface area of two alfisols and oxisol from Venezuela, Agrochimica Vol. 24: p. 5-6, 403-409. |