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1.A STUDY OF THE MUTUAL NON-INTERFERENCE EFFECT OF INORGANIC ION EXCHANGE IN SEAWATER Ⅰ. Ion Exchange Reactions of U(Ⅵ),Cr(Ⅱ),Ca,Mg with Hydrous Titanium Oxide in Seawater
海水中无机离子交换的互不相干作用 Ⅰ.海水中U(Ⅵ)、Cr(Ⅱ)、Ca、Mg与水合氧化钛的离子交换反应收藏指正
2.DETERMINATION OF TRACE Cu,Pb, Zn, Cd, Fe AND Mn IN SEAWATER BY ION-EXCHANGE AAS
离子交换—原子吸收光谱法测定海水中痕量铜、铅、锌、镉、铁、锰收藏指正
3.A new method of producing comparatively pure potassium sulphate from seawater using inartificial zeolite as the medium of ion exchange was especially introduced.
特别介绍了用天然沸石作为离子交换剂，从海水中制备较纯净的硫酸钾新工艺。收藏指正
4.EXCHANGE OF SEAWATER BETWEEN THE RED SEA AND THE GULF OF ADEN
红海及亚丁湾间之海水交换收藏指正
5.Water treatment: cleaning ion exchange resins; pure water production equipment; seawater desalination equipment.
水处理：清洗离子交换树脂；纯水生产设备；海水淡化设备。收藏指正
6.INTERFACIAL STEPWISE ION EXCHANGE ISOTHERMS OF COPPER, ZINC AND CADMIUM PARTITIONING ON CLAY MINERALS IN SEAWATER
海水中铜、锌、镉在粘土矿物上的分级离子交换等温线收藏指正
7.The main carbon modes of occurrence in the nepheloid layer are particulate organic carbon(POC),dissolved organic carbon(DOC), colloidal organic carbon(COC) and inorganic carbon, and the material exchange and transport of different carbon modes between nepheloid layer ambient seawater and sea bottom sediment take place under the actions of the bio-chemico-physico dynamic system, so the nepheloid layers play an important role in ocean carbon cycle and are a nonnegligible link in the entire ocean carbon cycle.
雾状层中碳的存在形态主要有颗粒有机碳(POC)、溶解有机碳(DOC)、胶体有机碳(COC)以及无机碳,雾状层与其上下海水之间、雾状层与海底表层沉积物之间不同形态碳在生物-化学-物理动力系统作用下不断发生物质交换与迁移,对海洋碳循环生物地球化学过程起重要的控制作用,是整个海洋碳循环的一个不可忽视的环节。收藏指正
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