Soil acidification and desertification


Fening Issac

Soil acidification is advantageous on account of alkaline soils, yet it corrupts land when it brings down crop productivity, soil natural action and builds soil weakness to defilement and disintegration. Soils are at first acidic and stay such when their parent materials are low in fundamental cations (calcium, magnesium, potassium and sodium). On parent materials more extravagant in weatherable minerals acidification happens when fundamental cations are drained from the dirt profile by precipitation or traded by the collecting of forest or agrarian yields. Soil acidification is sped up by the utilization of acid forming nitrogenous composts and by the impacts of acid precipitation. Deforestation is another reason for soil acidification, interceded by expanded filtering of soil supplements without tree canopies.

Share this article

Awards Nomination

Select your language of interest to view the total content in your interested language

Indexed In
  • Index Copernicus
  • Google Scholar
  • Sherpa Romeo
  • Open J Gate
  • Academic Keys
  • CiteFactor
  • Electronic Journals Library
  • OCLC- WorldCat
  • Advanced Science Index
  • Leipzig University Library
  • GEOMAR Library Ocean Research Information Access
  • OPAC
  • WZB
  • ZB MED
  • German National Library of Science and Technology
  • Secheresse Information and scientific resources
  • Paperpile
  • Life Science Portal Library
  • Academic Resource Index
  • University of Vechta Library
  • University of Hamburg Library
  • Disco ULB Muenster