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Fig. 1. Effect of redox processes on pH changes in ten wetland soils. The H+ generated was determined from the sum of H+ produced from oxidation of NH+4, Fe2+, and H2S determined in the samples (Table 2), with oxygen as the electron acceptor.





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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