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海洋微观世界的粒子。

The oceanic microcosm of particles.

出版信息

Science. 1977 Dec 9;198(4321):997-1009. doi: 10.1126/science.198.4321.997.

Abstract

Analyses of suspended particulate matter larger than 1 micrometer, filtered from thousands of liters of surface and deep waters during GEOSECS expeditions to the Atlantic and Pacific oceans, have provided new information on the nature and time scales of chemical processes associated with the particles. Trace element and radionuclide data show that particles scavenge trace elements such as Th, Pu, Fe, Pb, and Cu from the ocean column, thereby controlling their concentrations. For other elements, however, particles are a source: carbon and silicon, for example, are introduced at depths as sinking particles dissolve. Studies of both particulate concentrations by filtration of seawater and particulate fluxes by using sediment traps seem necessary to delineate the intricate nature of chemical processes in the oceans.

摘要

对在大西洋和太平洋的 GEOSECS 考察中从数千升地表水和深海水中过滤出来的大于 1 微米的悬浮颗粒物进行的分析,为与颗粒物有关的化学过程的性质和时间尺度提供了新的信息。痕量元素和放射性核素数据表明,颗粒物从海洋水柱中吸收了 Th、Pu、Fe、Pb 和 Cu 等痕量元素,从而控制了它们的浓度。然而,对于其他元素来说,颗粒物是一种来源:例如,随着下沉颗粒物的溶解,碳和硅被引入到深海中。通过过滤海水研究颗粒物浓度和使用沉积物捕集器研究颗粒物通量似乎是描绘海洋中化学过程复杂性质所必需的。

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