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The chemical distribution characteristics of variant form phosphorus in the seawater of the South China Sea

机译:南海海水中变型磷的化学分布特征

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摘要

According to two cruises investigation information in summer and winter during 1998 and1999, the phosphorous concentration distribution and changes of summer and winter were discussed pri-marily in the South China Sea. The results show that the phosphate concentration of surface seawater insummer is distinctly lower than that in winter, averaging 0.04 μmol/dm3 in summer and 0.35 μmol/dm3 in winter. The organic phosphorous concentration of surface seawater in summer is higher than thatin winter, averaging 0.12μmol/dm3 in summer and 0.04 μmol/dm3 in winter respectively. The season-al changes of total phosphorus are similar to phosphate, averaging 0.22 μmol/dm3 in summer and 0.61μmol/dm3 in winter respectively. In vertical direction, phosphate, TDP and TP content are the lowestin upper 50 m water column, and increase in linearity rapidly with water depth, increasing slowly under500 m, reach to maximum about 1 000 m, then decrease slightly with water depth increasing. The ver-tical distribution is typical in summer, and there is small dispersed for phosphorus concentration for thesame depth of different stations. However, in winter there is a large disperse for phosphate, TDP andTP, specifically for phosphate at 200 m at which the concentration is maximum. This result indicatesthat there are large differences in hydrology and biology conditions that affect largely the chemical envi-ronment of the South China Sea. The organic phosphorus is the predominant in surface seawater of theSouth China Sea, but the inorganic phosphorus is the predominant in layers below depth of 150 m. Theorganic phosphorus concentration in deep water usually decreases with water depth increasing. The or-ganic phosphorus in summer is remarkably more than that in winter because of the strong biology activi-ties in summer.
机译:根据1998年和1999年夏季和冬季的两次巡游调查信息,主要讨论了南中国海的磷浓度分布和夏季和冬季的变化。结果表明,夏季表层海水的磷酸盐浓度明显低于冬季,夏季平均为0.04μmol/ dm3,冬季平均为0.35μmol/ dm3。夏季地表海水的有机磷浓度高于冬季,夏季平均为0.12μmol/ dm3,冬季为0.04μmol/ dm3。总磷的季节变化与磷酸盐相似,夏季平均为0.22μmol/ dm3,冬季平均为0.61μmol/ dm3。在垂直方向上,磷酸盐,TDP和TP含量在上方50 m水柱中最低,并随水深呈线性增加,在500 m以下缓慢增加,最大达到约1000 m,然后随水深增加而略有下降。垂直分布在夏季是典型的,并且在不同站点的相同深度,磷浓度的分布很小。但是,在冬季,磷酸盐,TDP和TP的分散较大,尤其是浓度最大的200 m磷酸盐。该结果表明,水文和生物学条件存在很大差异,这在很大程度上影响了南中国海的化学环境。在南中国海的表层海水中,有机磷占主导地位,而深度在150 m以下的层中无机磷则占主导地位。深水中的有机磷浓度通常随着水深的增加而降低。由于夏季具有很强的生物学活性,夏季的有机磷明显高于冬季。

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  • 来源
    《海洋学报(英文版)》 |2003年第3期|385-394|共10页
  • 作者单位

    Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012,China;

    Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012,China;

    Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012,China;

    Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012,China;

    Key Laboratory of Submarine Geosciences of State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012,China;

    Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China;

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  • 原文格式 PDF
  • 正文语种 chi
  • 中图分类
  • 关键词

    the South China Sea; specific form phosphorus; biogeochemistry processes;

    机译:南海;特殊形式的磷;生物地球化学过程;
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