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沉积物离子交换法直接测定黄河口水体中溶解有机物的络合容量 被引量:3

DIRECT DETERMINATION OF COMPLEXING CAPACITY OF ORGANIC MATTERS DISSOLVED IN HUANGHE ESTUARY WATER BY THE HUANGHE ESTUARY SEDIMENT-ION EXCHANGE METHOD
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摘要 本文提出用黄河口沉积物为固体交换剂直接测定黄河口水体中溶解有机物的络合容量的一种新方法,其特点为:(1)不必假设“有机配位体和金属有机络合物与固体粒子不发生交换(或吸附)”;(2)运用普遍的吸附(交换)等温式;(3)在pH7—8范围内,δ-MnO_2的交换率(E%)高达近100,不能测得正常形式的等温线,无典型意义,而采用黄河口沉积物则无此缺点。 A new method to determine the complexing capacity of water (sea water and river water) by ion/coordination particle exchange is proposed with successful application to Huanghe Estuary water.1. Calculation of complexing capacity: Suppose the complexation between organic ligand A and inorganic ligand L(L = CO32- , HCO3-, OH-, SO42-) and trace metal Mn+ (Cu2+,Zn2+ and Cd2+ etc.) take place in Huanghe Estuary water. By mass equalibrium, the overall Cu(II) concentrationwhere α is α coefficent, with the expression of by mass equalibr-ium again,If there are more than two organic ligands [A(1)],…, [A(p)] in the system, thenBy Eqs. (1) and (5), we haveWhen ignoring the kind of A, and i equal 1,the terms [MA] and [Mn+] can be calculated as follows:By the ion/coordination particle exchange isothermaM can be expressed as (i = 1,2):The plot of [Mn+]/[MA] vs [Mn+], it[Mn+] and [MA] are given, should be straight line with a slope of 1/[A]total and intercept of 1/βA[A]total (Figs. 4 and 6).Van den Berg calculated the term [Mn+] by means of Langmuir equation, whereas we calculated it by means of the universal isotherm equation (9) from the theory of stepwise ion/coordination particle exchange, because the experiment really shows a stepwise type isotherm(Figs. 1 and 5). Also this calculation seems successful in two types of experiment carried out in this work.2. In order to simplify the calculation, two designed experiments were carried out: (1) Huanghe Estuary sediment served as ion exchanger; (2) Low pH condition (for example, pH = 3.0) Should be kept during the experiment that the exchange amount of organic matter or organic metal complexes on solid particle was kept as low as possible and then could be ignored in this case.As a result, the complexing capacity is [A]total = 0.49μm(pH = 8.0) and the stability constants are logβA = 8.45 (pH = 8.0) and logβA = 3.62(pH = 3. l),both of them are in good agreement with the previous literature data.3. The complexing capacity and overall apparent stability constants of Zn(II) and Cd(II) are shown in table 1.Tab. 1 The complexing capacity and overall apparent stability constants for Mn+-HES(Huanghe Estuary water systems)The complexing capacity and apparent stability constants of Mn+-HES(Huanghe Estuary systems) are in the order:Cu(II) > Zn(II) > Cd(II) This result agrees with the work in the literature.
机构地区 青岛海洋大学
出处 《海洋与湖沼》 CAS CSCD 北大核心 1990年第3期255-266,共12页 Oceanologia Et Limnologia Sinica
基金 国家自然科学基金
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参考文献3

  • 1张正斌,海洋物理化学,1989年
  • 2王修林,Chin J Oceanol Limnol,1988年,6卷,3期,258页
  • 3张正斌,海洋学报,1984年,6卷,3期,334页

同被引文献19

  • 1张正斌,刘莲生,郑士淮,张曼平.海洋物理化学进展[J].青岛海洋大学学报(自然科学版),1989,19(2):16-17. 被引量:14
  • 2杜青,文湘华,李莉莉,汤鸿霄.天然水体沉积物对重金属离子的吸附特性[J].环境化学,1996,15(3):199-206. 被引量:40
  • 3张正斌,刘莲生,孟晓光.海水中微量元素与固体粒子液-固界面离子/配位子交换的研究——Ⅻ.混合交换剂体系加和性研究[J]海洋与湖沼,1989(04).
  • 4张正斌,刘莲生,孟晓光,马炬珂,郭俊杰.作用的分级交换等温线[J]海洋与湖沼,1987(01).
  • 5刘莲生,张正斌,蔡卫君,张昊.海水中铜与针铁矿离子交换的动力学研究[J]海洋与湖沼,1986(05).
  • 6刘莲生,张正斌,郑士淮,杨桂朋,李旭,王伊明,陈敏仪,傅永法,陶锦清.海水中铜、锌、镉在粘土矿物上的分级离子交换等温线[J]海洋与湖沼,1986(04).
  • 7张正斌,刘莲生.海洋物理化学[M]科学出版社,1989.
  • 8张正斌,刘莲生,郑士淮,钟兆魁,薛军.海水中锌在针铁矿、赤铁矿和无定形水合氧化铁上液-固分配的一种新的化学模型[J]海洋与湖沼,1985(03).
  • 9吴瑜端.长江口海域有害重金属的转移机理 Ⅰ.转移规律的调查研究[J]海洋与湖沼,1978(02).
  • 10魏金玺.天然水中金属的络合容量及其测定[J]海洋湖沼通报,1984(02).

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