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ABSTRACT
Following nitrogen (N) transformations and movement in natural systems against a background of large amounts of this element requires use of isotopically labeled material which can be distinguished from that which is indigenous to the system. Methods are described for sampling and analyzing for labeled N in various components of the soil-plant-water system, and estimates of variability presented. The procedures described permitted construction of a balance sheet for long-term field trials with corn (Zea mays L.) in two locations in California. Unaccounted for losses ranged from 1% on Yolo fine sandy loam at 90 kg N/ha to > 50% in the coarse-textured Hanford sandy loam with high rates of N application. It was found possible to identify labeled N from 15N-depleted fertilizer in the soil organic fraction even after extensive dilution by using the isotopic composition of N in the corresponding layer of soil from unfertilized plots as the reference value rather than an overall mean.
Key Words: labeled N suction probes residual N nitrate
1 Contribution from the Dep. of Land, Air and Water Resources, Univ. of California, Davis, CA 95616. This work was supported by NSF Grants GI34733X, GI43664, AEN74-11136 A01, ENV76-10283, and PFR76-10283.
2 Professor of Soil Microbiology and Specialist in the Experiment Station, respectively.
Received for publication August 4, 1979.
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