THE CHEMISTRY OF THE HYDROGEN SULFIDE AND IRON SULFIDE SYSTEMS IN NATURAL WATERS

Morse J.W.; Millero F.J.; Cornwell J.C.; Rickard D.

dc.contributor.author	Morse J.W.
dc.contributor.author	Millero F.J.
dc.contributor.author	Cornwell J.C.
dc.contributor.author	Rickard D.
dc.date.accessioned	2020-04-17T00:43:22Z
dc.date.available	2020-04-17T00:43:22Z
dc.date.issued	1987
dc.identifier	https://elibrary.ru/item.asp?id=31395505
dc.identifier.citation	EARTH-SCIENCE REVIEWS, 1987, 24, 1, 1-42
dc.identifier.issn	0012-8252
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/16904
dc.description.abstract	Reduced sulfur compounds are ubiquitous components of anaerobic sediments and euxinic marine environments. They are primarily produced through a complex net of both chemically and biologically mediated reactions. This results in a wide variety of dissolved and solid inorganic and organic products.Much of the recent research effort in this area has focused on biogeochemical interactions and modelling sediment diagenesis. Several excellent reviews are available on these specific topics. However, relatively little attention has been paid to more basic inorganic chemistry of this system; the topic of this review.
dc.title	THE CHEMISTRY OF THE HYDROGEN SULFIDE AND IRON SULFIDE SYSTEMS IN NATURAL WATERS
dc.type	Статья