Unsaturated flow in an evaporative regime and cation exchange in soils

R. T. Raju, K. Jinno, Shin-Ichiro Wada

Research output: Contribution to journalArticle

Abstract

The data obtained show that the water moving upward by capillarity through the soil profile transfer soluble ions from the lower depths. Evaporation takes place just below the soil surface, where soluble salts tend to accumulate. The concentration of the soil solution increased drastically by precipitation of some soluble species. The cation exchange process is found to be influenced by the water chemistry in the vadose zone to a great extent. -from Authors

Original languageEnglish
Pages (from-to)263-269
Number of pages7
JournalUnknown Journal
Publication statusPublished - Jan 1 1993

Fingerprint

capillarity
unsaturated flow
vadose zone
water chemistry
soil profile
ion exchange
soil surface
evaporation
salt
ion
soil
water

All Science Journal Classification (ASJC) codes

  • Environmental Science(all)
  • Earth and Planetary Sciences(all)

Cite this

Raju, R. T., Jinno, K., & Wada, S-I. (1993). Unsaturated flow in an evaporative regime and cation exchange in soils. Unknown Journal, 263-269.

Unsaturated flow in an evaporative regime and cation exchange in soils. / Raju, R. T.; Jinno, K.; Wada, Shin-Ichiro.

In: Unknown Journal, 01.01.1993, p. 263-269.

Research output: Contribution to journalArticle

Raju, R. T. ; Jinno, K. ; Wada, Shin-Ichiro. / Unsaturated flow in an evaporative regime and cation exchange in soils. In: Unknown Journal. 1993 ; pp. 263-269.
@article{374f1c126ca04b768c8569bb11817ce7,
title = "Unsaturated flow in an evaporative regime and cation exchange in soils",
abstract = "The data obtained show that the water moving upward by capillarity through the soil profile transfer soluble ions from the lower depths. Evaporation takes place just below the soil surface, where soluble salts tend to accumulate. The concentration of the soil solution increased drastically by precipitation of some soluble species. The cation exchange process is found to be influenced by the water chemistry in the vadose zone to a great extent. -from Authors",
author = "Raju, {R. T.} and K. Jinno and Shin-Ichiro Wada",
year = "1993",
month = "1",
day = "1",
language = "English",
pages = "263--269",
journal = "Quaternary International",
issn = "1040-6182",
publisher = "Elsevier Limited",

}

TY - JOUR

T1 - Unsaturated flow in an evaporative regime and cation exchange in soils

AU - Raju, R. T.

AU - Jinno, K.

AU - Wada, Shin-Ichiro

PY - 1993/1/1

Y1 - 1993/1/1

N2 - The data obtained show that the water moving upward by capillarity through the soil profile transfer soluble ions from the lower depths. Evaporation takes place just below the soil surface, where soluble salts tend to accumulate. The concentration of the soil solution increased drastically by precipitation of some soluble species. The cation exchange process is found to be influenced by the water chemistry in the vadose zone to a great extent. -from Authors

AB - The data obtained show that the water moving upward by capillarity through the soil profile transfer soluble ions from the lower depths. Evaporation takes place just below the soil surface, where soluble salts tend to accumulate. The concentration of the soil solution increased drastically by precipitation of some soluble species. The cation exchange process is found to be influenced by the water chemistry in the vadose zone to a great extent. -from Authors

UR - http://www.scopus.com/inward/record.url?scp=0027804141&partnerID=8YFLogxK

UR - http://www.scopus.com/inward/citedby.url?scp=0027804141&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0027804141

SP - 263

EP - 269

JO - Quaternary International

JF - Quaternary International

SN - 1040-6182

ER -