The behavior of heavy metals in the mixing of river and sea water: the riverine part of an estuary and the migration of suspended and dissolved forms of heavy metals..

V. V. Anikiyev; O. S. Badtiyeva; A. A. Kotlyarova; N. I. Savel'yeva; O. V. Shevtsova; Y. N. Shumilin

The behavior of heavy metals in the mixing of river and sea water: the riverine part of an estuary and the migration of suspended and dissolved forms of heavy metals..

V. V. Anikiyev, O. S. Badtiyeva, A. A. Kotlyarova, N. I. Savel'yeva, O. V. Shevtsova, Y. N. Shumilin

Research output: Contribution to journal › Article › peer-review

Abstract

Studies have been made on the distributions of Fe, Mn, Sn and Cu in suspended and dissolved forms in the following systems: Razdol'naya River to Sea of Japan and Saigon River to S China Sea. It has been found that the suspensate is enriched in copper in the latter case at pH greater or equal to 7.6 and salinity 18-20%. Complexing with natural dissolved organic matter has an important effect on the migration of Fe, Mn and Cu in these estuaries. At salinities over 4%, the main migration forms for Fe and Mn in solution are as complexes with humic and fulvic acids.-Journal summary

Original language	English
Pages (from-to)	92-102
Number of pages	11
Journal	Geochemistry International
Volume	23
Issue number	1
State	Published - 1986
Externally published	Yes

Cite this

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title = "The behavior of heavy metals in the mixing of river and sea water: the riverine part of an estuary and the migration of suspended and dissolved forms of heavy metals..",

abstract = "Studies have been made on the distributions of Fe, Mn, Sn and Cu in suspended and dissolved forms in the following systems: Razdol'naya River to Sea of Japan and Saigon River to S China Sea. It has been found that the suspensate is enriched in copper in the latter case at pH greater or equal to 7.6 and salinity 18-20%. Complexing with natural dissolved organic matter has an important effect on the migration of Fe, Mn and Cu in these estuaries. At salinities over 4%, the main migration forms for Fe and Mn in solution are as complexes with humic and fulvic acids.-Journal summary",

author = "Anikiyev, {V. V.} and Badtiyeva, {O. S.} and Kotlyarova, {A. A.} and Savel'yeva, {N. I.} and Shevtsova, {O. V.} and Shumilin, {Y. N.}",

year = "1986",

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volume = "23",

pages = "92--102",

journal = "Geochemistry International",

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T1 - The behavior of heavy metals in the mixing of river and sea water

T2 - the riverine part of an estuary and the migration of suspended and dissolved forms of heavy metals..

AU - Anikiyev, V. V.

AU - Badtiyeva, O. S.

AU - Kotlyarova, A. A.

AU - Savel'yeva, N. I.

AU - Shevtsova, O. V.

AU - Shumilin, Y. N.

PY - 1986

Y1 - 1986

N2 - Studies have been made on the distributions of Fe, Mn, Sn and Cu in suspended and dissolved forms in the following systems: Razdol'naya River to Sea of Japan and Saigon River to S China Sea. It has been found that the suspensate is enriched in copper in the latter case at pH greater or equal to 7.6 and salinity 18-20%. Complexing with natural dissolved organic matter has an important effect on the migration of Fe, Mn and Cu in these estuaries. At salinities over 4%, the main migration forms for Fe and Mn in solution are as complexes with humic and fulvic acids.-Journal summary

AB - Studies have been made on the distributions of Fe, Mn, Sn and Cu in suspended and dissolved forms in the following systems: Razdol'naya River to Sea of Japan and Saigon River to S China Sea. It has been found that the suspensate is enriched in copper in the latter case at pH greater or equal to 7.6 and salinity 18-20%. Complexing with natural dissolved organic matter has an important effect on the migration of Fe, Mn and Cu in these estuaries. At salinities over 4%, the main migration forms for Fe and Mn in solution are as complexes with humic and fulvic acids.-Journal summary

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M3 - Artículo

SN - 0016-7029

VL - 23

SP - 92

EP - 102

JO - Geochemistry International

JF - Geochemistry International

IS - 1

ER -

The behavior of heavy metals in the mixing of river and sea water: the riverine part of an estuary and the migration of suspended and dissolved forms of heavy metals..

Abstract

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