非洲土壤原位比湿和有效含水量的判别土壤因子

Agronomie Pub Date : 2004-03-01 DOI:10.1051/AGRO:2004002
S. Valet, P. Allemand
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引用次数: 2

摘要

地下水和作物可利用水的管理需要了解土壤的水文行为。从塞内加尔北部到南部进行了一项约5度纬度的研究,涵盖了大范围的土壤因素和各种气候、地质和地貌条件。103种土壤的1387个层样以0.1 m的增量从地表到2 m深度。研究的土壤学性质为粘土+粉粒含量、容重、交换性Na +和ph。水力性质为最小含水量、田间容量和有效含水量。主成分分析结果表明,土壤结构、最小含水量和田间容量、有效含水量和pH值的重要性依次递减。除有效含水量外,所有混合层、按层分组的土壤和两种土壤(arennosol和Ferralsol)的最小含水量预测值和实测值与田间容量数据吻合良好。而有效含水量可以通过统计计算的方法,对每一层的纹理类进行分组。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Discriminant pedological factors of in situ specific moisture and available water content of African soils
The management of groundwater and crop-available water requires the knowledge of the hydrological behaviour of soils. A study was carried out from North to South Senegal on about 5 degrees of latitude, which cover a large range of pedological factors and various climatic, geologic and geomorphologic conditions. 1387 layer samples of 103 soils were taken from the surface to 2 m depth by 0.1 m-deep increments. The studied pedological properties were clay + silt content, bulk density, exchangeable Na + and pH. The hydraulic properties were the minimum moisture content, the field capacity and the available water content. Principal component analysis shows that the main factors, the texture, the minimum moisture content and field capacity, the available water content and the pH were in a decreasing order of importance. A good agreement between predicted and measured values of the minimum moisture content and the field capacity data, except for the available water content, was found for all mixed layers, for soils grouped according to their layers and for two soils (Arenosol and Ferralsol). However, the available water content can be calculated by statistical calculation by the grouping of textural classes for each layer.
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