Skip Navigation


JXB Advance Access originally published online on March 1, 2006
Journal of Experimental Botany 2006 57(5):1017-1023; doi:10.1093/jxb/erj108
This Article
Right arrow Full Text Freely available
Right arrow FREE Full Text (PDF) Freely available
Right arrow All Versions of this Article:
57/5/1017    most recent
erj108v1
Right arrow E-letters: Submit a response
Right arrow Alert me when this article is cited
Right arrow Alert me when E-letters are posted
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Similar articles in PubMed
Right arrow Alert me to new issues of the journal
Right arrow Add to My Personal Archive
Right arrow Download to citation manager
Right arrow Search for citing articles in:
ISI Web of Science (22)
Right arrowRequest Permissions
Right arrow Disclaimer
Google Scholar
Right arrow Articles by Rengasamy, P.
Right arrow Search for Related Content
PubMed
Right arrow PubMed Citation
Right arrow Articles by Rengasamy, P.
Agricola
Right arrow Articles by Rengasamy, P.
Social Bookmarking
 Add to CiteULike   Add to Connotea   Add to Del.icio.us  
What's this?

© The Author [2006]. Published by Oxford University Press [on behalf of the Society for Experimental Biology]. All rights reserved. For Permissions, please e-mail: journals.permissions@oxfordjournals.org

RESEARCH PAPER

World salinization with emphasis on Australia

Pichu Rengasamy*

Soil and Land Systems, School of Earth and Environmental Sciences, The University of Adelaide, Waite Campus, PMB 1, Glen Osmond, SA 5064, Australia

* E-mail: pichu.rengasamy{at}adelaide.edu.au

Salinization is the accumulation of water-soluble salts in the soil solum or regolith to a level that impacts on agricultural production, environmental health, and economic welfare. Salt-affected soils occur in more than 100 countries of the world with a variety of extents, nature, and properties. No climatic zone in the world is free from salinization, although the general perception is focused on arid and semi-arid regions. Salinization is a complex process involving the movement of salts and water in soils during seasonal cycles and interactions with groundwater. While rainfall, aeolian deposits, mineral weathering, and stored salts are the sources of salts, surface and groundwaters can redistribute the accumulated salts and may also provide additional sources. Sodium salts dominate in many saline soils of the world, but salts of other cations such as calcium, magnesium, and iron are also found in specific locations. Different types of salinization with a prevalence of sodium salts affect about 30% of the land area in Australia. While more attention is given to groundwater-associated salinity and irrigation salinity, which affects about 16% of the agricultural area, recent investigations suggest that 67% of the agricultural area has a potential for ‘transient salinity’, a type of non-groundwater-associated salinity. Agricultural soils in Australia, being predominantly sodic, accumulate salts under seasonal fluctuations and have multiple subsoil constraints such as alkalinity, acidity, sodicity, and toxic ions. This paper examines soil processes that dictate the exact edaphic environment upon which root functions depend and can help in research on plant improvement.

Key words: Dry-land salinity, irrigation salinity, salinity in Australia, soil processes affecting salinity effects, transient salinity, world salinization


Add to CiteULike CiteULike   Add to Connotea Connotea   Add to Del.icio.us Del.icio.us    What's this?


This article has been cited by other articles:


Home page
J HeredHome page
J.-D. Lee, J. G. Shannon, T. D. Vuong, and H. T. Nguyen
Inheritance of Salt Tolerance in Wild Soybean (Glycine soja Sieb. and Zucc.) Accession PI483463
J. Hered., June 25, 2009; (2009) esp027v2.
[Abstract] [Full Text] [PDF]


Home page
J Exp BotHome page
F. Queiros, N. Fontes, P. Silva, D. Almeida, M. Maeshima, H. Geros, and F. Fidalgo
Activity of tonoplast proton pumps and Na+/H+ exchange in potato cell cultures is modulated by salt
J. Exp. Bot., March 1, 2009; 60(4): 1363 - 1374.
[Abstract] [Full Text] [PDF]


Home page
Crop Sci.Home page
J.-D. Lee, S. L. Smothers, D. Dunn, M. Villagarcia, C. R. Shumway, T. E. Carter Jr., and J. G. Shannon
Evaluation of a Simple Method to Screen Soybean Genotypes for Salt Tolerance
Crop Sci., November 24, 2008; 48(6): 2194 - 2200.
[Abstract] [Full Text] [PDF]


Home page
jashsHome page
G. Niu and D. S. Rodriguez
Responses of Growth and Ion Uptake of Four Rose Rootstocks to Chloride- or Sulfate-dominated Salinity
J. Amer. Soc. Hort. Sci., September 1, 2008; 133(5): 663 - 669.
[Abstract] [Full Text] [PDF]


Home page
Plant Physiol.Home page
N. C. Collins, F. Tardieu, and R. Tuberosa
Quantitative Trait Loci and Crop Performance under Abiotic Stress: Where Do We Stand?
Plant Physiology, June 1, 2008; 147(2): 469 - 486.
[Full Text] [PDF]


Home page
J Exp BotHome page
S. Huang, W. Spielmeyer, E. S. Lagudah, and R. Munns
Comparative mapping of HKT genes in wheat, barley, and rice, key determinants of Na+ transport, and salt tolerance
J. Exp. Bot., March 5, 2008; (2008) ern033v1.
[Abstract] [Full Text] [PDF]



Disclaimer: Please note that abstracts for content published before 1996 were created through digital scanning and may therefore not exactly replicate the text of the original print issues. All efforts have been made to ensure accuracy, but the Publisher will not be held responsible for any remaining inaccuracies. If you require any further clarification, please contact our Customer Services Department.