SOME ASPECTS ON WATER REPELLENCY OF SOILS
スポンサーリンク
概要
- 論文の詳細を見る
The changes of water repellency of soils, such as peat soil and volcanic ash soil, were measured with the one water drop method. Bibai peat soil and A_0 or A_1 horizons of the forest soil were difficult to wet when they were dried at 105℃, and it became wettable when it was heated to temperatures above 250℃. The peat soil heated to 200℃ was wettable when the puddled soil was shrinked and dried, on the other hand it was nonwettable when it was crushed or sieved. By heating to temperatures above 250℃, all samples became completely wettable. Bibai peat soil was more nonwettable when it was treated with hydrogen peroxide. It was also found that forest soil was more nonwettable than the cultivated soils even if the organic matter content of both soils were nearly equal.
- 社団法人日本土壌肥料学会の論文
著者
-
Yokoi Hajime
National Institute Of Agricultural Sciences
-
Nakaya Norio
National Institute Of Agricultural Sciences
-
MOTOMURA Satoru
National Institute of Agricultural Sciences
関連論文
- THE METHOD FOR MEASURING OF WATER REPELLENCY OF SOIL
- SOME ASPECTS ON WATER REPELLENCY OF SOILS
- PRESUMPTIVE EFFECT OF AGGREGATES ON TEXTURAL CLASSIFICATION
- FRACTIONATION METHOD OF FERROUS IRON IN PADDY SOIL
- THE RELATIONSHIP BETWEEN FERROUS IRON FORMATION AND NITROGEN METABOLISM IN SOIL
- EFFECT OF ORGANIC MATTERS ON THE FORMATION OF FERROUS IRON IN SOILS
- SOIL STRUCTURE DEVELOPMENT IN ARIAKE POLDER SOILS IN RELATION TO IRON FORMS
- THEORETICAL ANALYSIS OF TEXTURAL CLASSIFICATION FOR THREE-FRACTION SYSTEM
- STUDIES ON THE GLEY FORMATION OF SOILS I. : On the Mechanism of the Formation of Active Ferrous Iron in Soils
- RELATIONSHIP BETWEEN SOIL COHESION AND SHEAR STRENGTH
- THEORETICAL ANALYSIS OF PARTICLE-SIZE DISTRIBUTION : An Approximation to Continuous System
- CHARACTERISTICS OF FERROUS IRON FORMS IN PADDY SOIL WITH REFERENCE TO DEVELOPMENT OF THE SOIL PROFILE