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


     


Published in J Environ Qual 15:260-265 (1986)
© 1986 American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
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
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lang, F. J.
Right arrow Articles by Crane, N. L.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Lang, F. J.
Right arrow Articles by Crane, N. L.
Agricola
Right arrow Articles by Lang, F. J.
Right arrow Articles by Crane, N. L.

Boron Deposition on Soil and Native Vegetation from Geothermal Emissions1

F. J. Lang, F. T. Bingham, F. F. Hendrix and N. L. Crane2

ABSTRACT

Boron deposition, soil B, and foliage B were sampled in a field study around two geothermal generating units with different operating histories; the study also determined relative sensitivities of several native tree species to B in soil and foliage. Boron emissions from the older cooling tower, operational for 11 yr, were nearly 5 times greater than emissions from the newer cooling tower, operational for 2.5 yr. This difference was due to substantially greater B concentrations in circulating water at the older unit. Boron deposition was as great as 129.6 kg ha–1 yr–1 at the older unit and 4.2 kg ha–1 yr–1 at the newer unit. Soil B (saturation extract) was as great as 44.0 mg L–1 at the older unit and 0.6 mg L–1 at the newer unit. At a given rate of B deposition, soil B was more than 4 times greater at the older unit due to its longer operating history. At a given soil B level, the deciduous bigleaf maple (Acer macrophyllum Pursh) contained double the foliage B of the broadleaf evergreen, interior live oak (Quercus wislizeni A. DC.), and about 5 times greater foliage B than the conifer, Digger pine (Pinus sabiniana Dougl.). Foliage B thresholds for detectable levels of visible injury due to B toxicity were about 500 mg kg–1 for both bigleaf maple and interior live oak. These relationships suggest that more rapid B accumulation is responsible for higher levels of visible injury due to B in bigleaf maples than in other native tree species.

Key Words: bigleaf maple • interior live oak • Digger pine • visible foliage injury • cooling tower drift • boron toxicity


NOTES

1 Research supported by Pacific Gas and Electric Co., Dep. of Engineering Research, San Ramon, CA 94583.

2 Environmental Scientist, Jones & Stokes Associates, Sacramento, CA 95816; Professor of Soil Science, Univ. of California, Riverside; Professor of Plant Pathology, Univ. of Georgia; and Biologist, Pacific Gas and Electric Co., San Ramon, CA, respectively.

Received for publication August 23, 1985.





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
Soil Science Society of America Journal
Copyright © 1986 by the American Society of Agronomy, Crop Science Society of America, and Soil Science Society of America.