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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
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.
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