@article{
 title = {Denitrification in Lake 227 During Summer Stratification},
 type = {article},
 year = {1980},
 identifiers = {[object Object]},
 keywords = {L227,bacteria,denitrification,eutrophication,lake mixing,nutrient cycling,nutrients},
 pages = {506-512},
 volume = {37},
 id = {966fb229-bb3f-3639-9340-01f55fcf6000},
 created = {2019-07-11T22:03:19.609Z},
 file_attached = {true},
 profile_id = {3c181434-ae75-3e95-a723-2bfcc2f14c0b},
 group_id = {db3318bf-b2fb-3b86-9f1d-17188c0ddfa3},
 last_modified = {2020-11-03T17:05:52.289Z},
 read = {true},
 starred = {false},
 authored = {false},
 confirmed = {true},
 hidden = {false},
 citation_key = {Chan2008},
 private_publication = {false},
 abstract = {In situ denitrification in Lake 227 was assayed by using 15N-labeled N0₃- during summer stratification periods in 1973,1974, and 1975. Dissolved oxygen and NO₃- concentrations were the main factors controlling denitrification in the water column and in sediments. The epilimnetic sediment-water interface was a more significant site of natural denitrification when compared to the oxygen-limiting (dissolved oxygen less than 0.2 mg/L) thermocline and the anoxic hypolimnion. Epilimnetic sediment denitrification rates averaged about 15 mg N.m-2·d-1. Nearly all of the NO₃- that mixed into the surficial sediments was denitrified. Alone, epilimnetic denitrification removed 1.4% of the NO₃- added annually. Below the euphotic zone, sediments would provide an efficient sink for N0₃--N without sirnuBtaneous initiation of eutrophication.},
 bibtype = {article},
 author = {Chan, Y. K. and Campbell, N. E. R.},
 journal = {Canadian Journal of Fisheries and Aquatic Sciences},
 number = {3}
}

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