SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 25 January 2008
Published in Soil Sci Soc Am J 72:431-441 (2008)
DOI: 10.2136/sssaj2006.0117N
© 2008 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Google Scholar
Right arrow Articles by Chaudhari, S. K.
Right arrow Articles by Kundu, D. K.
PubMed
Right arrow Articles by Chaudhari, S. K.
Right arrow Articles by Kundu, D. K.
Agricola
Right arrow Articles by Chaudhari, S. K.
Right arrow Articles by Kundu, D. K.
Related Collections
Right arrow Soil Physics
Right arrow Soil Analysis
Right arrow Soil Methods/Instrumentation

SOIL & WATER MANAGEMENT & CONSERVATION NOTE

Rapid Textural Analysis for Saline and Alkaline Soils with Different Physical and Chemical Properties

S. K. Chaudhari*, R. Singh and D. K. Kundu

Coordinating Unit on Water Manage., Water Tech. Centre for Eastern Region, P.O. SE Railway Project, Chandrasekharpur, Bhubaneswar 751 023, Orissa, India

* Corresponding author (surchaudhari{at}hotmail.com).

In most soil testing laboratories, textural analysis is performed by the pipette method (PM) or by hydrometer. Objectives of this study were (i) to evaluate simplified methods that can be used for soils of various textures, and (ii) to modify a rapid method for reliable and accurate textural analysis of saline and alkaline soils. One hundred soils were collected from different agro-ecological regions of India. Coefficients of variation for sand, silt, and clay of soil samples by the rapid method varied across a range of 0 to 5% with a mean value <3% for all soils. Absolute differences between the PM and the rapid method for sand, silt, and clay fractions ranged from –1.8 to 1.7, –1.8 to 5.3, and –2.9 to 1.8%, with averages across the sites of –0.04, 2.92, and –6.52%, respectively. Among various methods, regression analysis between the rapid and pipette methods produced the highest coefficient of determination (r2) values of 0.9989, 0.9927, and 0.9930 for sand, silt, and clay fractions, respectively. A rapid method with modified sodium hexametaphosphate concentrations and soil shaking periods produced mean, standard error, and standard deviation values very close to the PM, with r2 values >0.99 with small intercepts <0.5, <0.3, and <0.7 for saline, saline–alkaline, and alkaline soils, respectively. The rapid method with proposed modifications provides the most accurate and fast estimation of texture for saline–alkaline soils.

Abbreviations: HMP, sodium hexametaphosphate • PM, pipette method • POM, particulate organic matter







HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Vadose Zone Journal Journal of Plant Registrations
Journal of Natural Resources
and Life Sciences Education
Journal of
Environmental Quality
Copyright © 2008 by the Soil Science Society of America.