SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published online 1 July 2008
Published in Soil Sci Soc Am J 72:1163-1173 (2008)
DOI: 10.2136/sssaj2007.0268
© 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 Sikora, F. J.
Right arrow Articles by Moore, K. P.
PubMed
Right arrow Articles by Sikora, F. J.
Right arrow Articles by Moore, K. P.
Agricola
Right arrow Articles by Sikora, F. J.
Right arrow Articles by Moore, K. P.
Related Collections
Right arrow Soil pH
Right arrow Soil Analysis
Right arrow Soil Chemistry

NUTRIENT MANAGEMENT & SOIL & PLANT ANALYSIS

The Moore–Sikora Buffer for Lime Requirement Determinations

F. J. Sikoraa,* and K. P. Mooreb

a Univ. of Kentucky, Soil Testing Lab., 103 Regulatory Service Bldg., Lexington, KY 40546-0275
b Clemson University, Agricultural Service Lab., 171 Old Cherry Rd., Clemson, SC 29634

* Corresponding author (fsikora{at}uky.edu).

Paranitrophenol in the Adams–Evans (AE) buffer used for determining lime requirement (LR) is considered a hazardous chemical due to its toxicity. The Moore–Sikora (MS) buffer, which mimics AE soil-buffer pH, was developed without hazardous chemicals and is currently used for routine soil testing at Clemson University. The MS buffer was designed by considering probable chemicals with pKa values in the desired pH range, potential reaction of the components with soil, and longevity of the buffer during storage. Boric acid, 3-(N-morpholino)propanesulfonic acid (MOPS), and 2-(N-morpholino)ethanesulfonic acid hydrate (MES) were considered for the new buffer. Once chemicals were identified, a technique of finding appropriate concentrations was utilized by using an equation that could predict the acid titration of a buffer and refining pKa and concentration values until a match was found with measured pH titrations of the AE buffer. The MS buffer contains 212, 131, and 34.8 mmol L–1 of B(OH)3, MOPS, and MES, respectively. The buffer also contains 200 mmol L–1 KOH and 1 mol L–1 KCl. The MS buffer was compared with the AE buffer for determining soil-buffer pH values on 222 South Carolina soils and 41 North American Proficiency Testing Program soils. The MS soil-buffer pH was strongly related to AE soil-buffer pH (r2 > 0.98). Soil-buffer pH was slightly less with MS buffer than AE buffer, with a mean difference of 0.03 pH units. The lower soil-buffer pH with MS buffer caused a slightly higher LR than the AE buffer, with a mean difference of 0.34 Mg ha–1 on South Carolina soils. Forty-four percent of the samples indicating a need for lime did not have a difference in LR between the two buffers. The slightly higher LR with the MS buffer on some of the samples is not expected to raise soil pH too high above target pH values.

Abbreviations: AE, Adams–Evans • LR, lime requirement • MES, 2-(N-morpholino)ethanesulfonic acid hydrate • MOPS, 3-(N-morpholino)propanesulfonic acid • MS, Moore–Sikora • NAPT, North American Proficiency Testing.







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 © 2008 by the Soil Science Society of America.