论文部分内容阅读
THEQUANTITATIVETREATMENTOFEXCHANGEADSORPTIONISOTHERMSOFSURFACELAYERSEDIMENTFROMTHESOUTHCHINASEA海水中液-固界面间的交换吸附对微量元素的存在形式和分布及生物可给性起着决定作用，具有广大表面的海底沉积物对微量金属的交换吸附已被广泛认为是使微量金属在海水中保持
THEQUANTITATIVETREATMENTOFEXCHANGEADSORPTIONISOTHERMSOFSURFACELAYERSEDIMENTFROMTHESOUTHCHINASEA The exchange adsorption between the liquid-solid interface in seawater plays a decisive role in the existence and distribution of trace elements and in the bioavailability. The exchange adsorption of trace metals on seafloor sediments with a wide range of surfaces has been widely recognized as the result of micro- Keep in the sea water