Amelioration of subsoil acidity in a nonallophanic Andosol by surface application of organic calcium salts

Citation
K. Inoue et al., Amelioration of subsoil acidity in a nonallophanic Andosol by surface application of organic calcium salts, SOIL SCI PL, 47(1), 2001, pp. 113-122
Citations number
22
Categorie Soggetti
Agriculture/Agronomy
Journal title
SOIL SCIENCE AND PLANT NUTRITION
ISSN journal
00380768 → ACNP
Volume
47
Issue
1
Year of publication
2001
Pages
113 - 122
Database
ISI
SICI code
0038-0768(200103)47:1<113:AOSAIA>2.0.ZU;2-Z
Abstract
The effects of surface application of organic Ca-salts on the amelioration of the subsoil acidity in a nonallophanic Andosol distributed in Hiroshima Prefecture were studied by a model experiment with columns. Consequently, t he effects of inorganic Ca-salts were also examined compared with those of organic Ca-salts. Topsoil treatment with carbonate and nitrate did not lead to a substantial amelioration of the subsoil acidity. In the sulfate treat ment, approximately 64% of Ca applied to the topsoil was distributed unifor mly in the 10-50 cm subsoil layers after the 20th irrigation (800 mm as rai nfall). However, there was a large amount of exchangeable Al in the subsoil and the subsoil pH was obviously lower than that of the control. Thus, the se three inorganic Ca salts were unsuitable for ameliorating the subsoil ac idity in the nonallophanic Andosol used in this study. In the EDTA, citrate , and acetate treatments, Ca was distributed in the subsoil though its cont ent decreased with the soil depth and the total amount of Ca distributed in the 10-50 cm subsoil layers was approximately 63, 44, and 55% of that appl ied to the topsoil, respectively. In addition, almost all of the Ca distrib uted in the subsoil was in an exchangeable form. In the EDTA treatment, the subsoil pH exceeded 6.0 and the amount of exchangeable Al was very low. Al though citrate and acetate are not as effective as EDTA, these Ca-salts als o led to a decrease of the content of exchangeable Al in the 10-50 cm subso il layers and to an increase of pH in the 10-30 cm subsoil layers.