期刊
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
卷 121, 期 5, 页码 3659-3667出版社
AMER GEOPHYSICAL UNION
DOI: 10.1002/2016JC011651
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For 50 years, ocean scientists have represented deep sea biogeochemical rates as a temperature independent function of depth with form R = R(0)e(-alpha z) where z is depth in km. We show this resembles, but is not an identity for, a form of the classical Arrhenius equation K=Ae(-Ea/RT) where T is temperature in Kelvins, R is the gas constant (8.314 JK(-1) mol(-1)), and A is a preexponential factor. For a deep Sargasso Sea data set, we find oxygen consumption rates are accurately represented by an Arrhenius process with apparent activation energy of 86.5 kJ mol(-1), and Q(10)=3.63.
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