透光带
硝酸盐
海洋学
亚热带
海水
浮游生物
环境科学
新产品
停留时间(流体动力学)
地质学
生态学
浮游植物
营养物
生物
岩土工程
作者
Richard W. Eppley,Wolfgang Koeve
标识
DOI:10.4319/lo.1990.35.8.1781
摘要
Nitrate concentration was measured in seawater samples from the euphotic zone at the beginning and end of 12‐h, daytime, in situ incubations. The changes in concentration are considered to be measurements of new production. During periods of 2–3 weeks in March–April 1989, important time scales for NO 3 − input to the euphotic zone (i.e. residence times) and new production were ~26 d at 18°N, 31°W and ~10 d near 33°N, 21°W. The average rate of NO 3 − use in the two areas was 2.63 and 0.62 mmol N m −2 (12 h) −1 , or, in carbon equivalents 209 and 49 mg C m −2 d −1 , respectively. These values bracket the large‐scale estimate by Jenkins of new production in the nearby beta triangle of 150 mg C m −2 d −1 .
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