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


     


This Article
Right arrow Figures Only
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
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 Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (1)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Liu, M.
Right arrow Articles by Vendrell, P. F.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Liu, M.
Right arrow Articles by Vendrell, P. F.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Liu, M.
Right arrow Articles by Vendrell, P. F.
Related Collections
Right arrow Soil pH
Right arrow Soil Analysis
Right arrow Soil Chemistry
Published in Soil Sci. Soc. Am. J. 69:522-530 (2005).
© 2005 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA

Division S-8—Nutrient Management & Soil & Plant Analysis

Soil Lime Requirement by Direct Titration with a Single Addition of Calcium Hydroxide

Min Liu, D. E. Kissel*, M. L. Cabrera and P. F. Vendrell

Dep. of Crop and Soil Sciences and Agricultural and Environmental Services Labs., 2400 College Station Road, Univ. of Georgia, Athens, GA 30602

* Corresponding author (dkissel{at}uga.edu)

Direct titration of acid surface soils is often used to measure soil acidity. However, titration has not been used for routine determination of the lime requirement (LR) in soil testing laboratories, because it is too time-consuming, requiring multiple additions of base and long equilibration times between additions. Since soil pH as a function of added base can be described well by a linear equation, titration may be adopted by soil testing laboratories using a minimum number of base additions. Our objective was to evaluate the accuracy of a simplified titration procedure, based on an initial pH reading and a second reading following the addition of one dose of Ca(OH)2, followed by extrapolation to the target pH. Seventeen soils were titrated with Ca(OH)2 in both water and 0.01 M CaCl2 with a 30-min interval between additions. The slopes from the first two data points of the titration in water were frequently in error for estimation of the slopes regressed by all data points to pH 6.5. However, the first two data points in the 0.01 M CaCl2 titration were found to be more reliable for estimating the slopes. Both the initial pH in water and in 0.01 M CaCl2 were used to calculate the LR with the two-point slope in 0.01 M CaCl2. The LR predicted using the initial pH in 0.01 M CaCl2 gave better estimates of the LR than the initial water pH when compared with the standard 3-d Ca(OH)2 incubation. A linear regression of LR by the single addition method in 0.01 M CaCl2 (Y) on LR determined with the 3-d Ca(OH)2 incubation (X) gave the linear equation Y = 0.88 X, r2 = 0.93. It is concluded that the LR predictions with the single addition method in 0.01 M CaCl2 are sufficiently accurate to justify further evaluation under routine laboratory conditions.

Abbreviations: A-E, Adams-Evans • CEC, cation exchange capacity • LR, lime requirement • OAc, acetate • SMP, Shoemaker–McLean–Pratt




This article has been cited by other articles:


Home page
Soil Sci.Home page
F. J. Sikora and K. P. Moore
The Moore-Sikora Buffer for Lime Requirement Determinations
Soil Sci. Soc. Am. J., July 1, 2008; 72(4): 1163 - 1173.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
C. B. Godsey, G. M. Pierzynski, D. B. Mengel, and R. E. Lamond
Evaluation of Common Lime Requirement Methods
Soil Sci. Soc. Am. J., April 5, 2007; 71(3): 843 - 850.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
F. J. Sikora
A Buffer that Mimics the SMP Buffer for Determining Lime Requirement of Soil
Soil Sci. Soc. Am. J., February 2, 2006; 70(2): 474 - 486.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2005 by the Soil Science Society of America.