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Factors affecting the formation and oxidation of sulphides in a polluted estuary
Factors affecting the formation and destruction of sulphide in the Thames Estuary have been discussed. Measurements of oxidation-reduction potentials show that the effect of oxygen in the water on conditions in deposits of mud is limited to the surface layer. The rate of formation of sulphide increa...
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Published in: | The Journal of hygiene 1954-06, Vol.52 (2), p.194-210 |
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description | Factors affecting the formation and destruction of sulphide in the Thames Estuary have been discussed. Measurements of oxidation-reduction potentials show that the effect of oxygen in the water on conditions in deposits of mud is limited to the surface layer. The rate of formation of sulphide increases with temperature, doubling approximately for each 10° C. rise. Reduction of sulphate to sulphide will occur at temperatures as low as 5° C., but even at 25° C. is inhibited by traces of dissolved oxygen. Mud in suspension in the estuary can produce as much sulphide as compact layers of similar mud which might be more anaerobic. Oxidation of sulphide in the Thames Estuary is shown to be of a purely chemical nature; the rate of oxidation, when oxygen is present, is increased by the presence of suspended matter and iron. In the Thames Estuary, however, the rate is limited by the rate at which oxygen enters the water. Much of the experimental work described in this paper was carried out by Miss A. Laird, Mr A. E. Sutton and Mr R. B. Peel of this Laboratory. The paper is published by permission of the Department of Scientific and Industrial Research. |
doi_str_mv | 10.1017/S0022172400027406 |
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B.</creator><creatorcontrib>Wheatland, A. B.</creatorcontrib><description>Factors affecting the formation and destruction of sulphide in the Thames Estuary have been discussed. Measurements of oxidation-reduction potentials show that the effect of oxygen in the water on conditions in deposits of mud is limited to the surface layer. The rate of formation of sulphide increases with temperature, doubling approximately for each 10° C. rise. Reduction of sulphate to sulphide will occur at temperatures as low as 5° C., but even at 25° C. is inhibited by traces of dissolved oxygen. Mud in suspension in the estuary can produce as much sulphide as compact layers of similar mud which might be more anaerobic. Oxidation of sulphide in the Thames Estuary is shown to be of a purely chemical nature; the rate of oxidation, when oxygen is present, is increased by the presence of suspended matter and iron. In the Thames Estuary, however, the rate is limited by the rate at which oxygen enters the water. Much of the experimental work described in this paper was carried out by Miss A. Laird, Mr A. E. Sutton and Mr R. B. Peel of this Laboratory. 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B.</creatorcontrib><title>Factors affecting the formation and oxidation of sulphides in a polluted estuary</title><title>The Journal of hygiene</title><addtitle>J. Hyg</addtitle><description>Factors affecting the formation and destruction of sulphide in the Thames Estuary have been discussed. Measurements of oxidation-reduction potentials show that the effect of oxygen in the water on conditions in deposits of mud is limited to the surface layer. The rate of formation of sulphide increases with temperature, doubling approximately for each 10° C. rise. Reduction of sulphate to sulphide will occur at temperatures as low as 5° C., but even at 25° C. is inhibited by traces of dissolved oxygen. Mud in suspension in the estuary can produce as much sulphide as compact layers of similar mud which might be more anaerobic. Oxidation of sulphide in the Thames Estuary is shown to be of a purely chemical nature; the rate of oxidation, when oxygen is present, is increased by the presence of suspended matter and iron. In the Thames Estuary, however, the rate is limited by the rate at which oxygen enters the water. Much of the experimental work described in this paper was carried out by Miss A. Laird, Mr A. E. Sutton and Mr R. B. Peel of this Laboratory. The paper is published by permission of the Department of Scientific and Industrial Research.</description><subject>Bottles</subject><subject>Environmental Pollution</subject><subject>Estuaries</subject><subject>Hazardous Substances</subject><subject>Hydrogen</subject><subject>Mud</subject><subject>Old Medline</subject><subject>Oxidation</subject><subject>Oxidation-Reduction</subject><subject>Oxygen</subject><subject>River water</subject><subject>Sea water</subject><subject>Sewage</subject><subject>Sulfate reducing bacteria</subject><subject>Sulfides</subject><subject>Water Supply</subject><issn>0022-1724</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1954</creationdate><recordtype>article</recordtype><recordid>eNp9kUtv1DAUhb0A0VL4AUgIecUu1I6dON4goaEtlaaivMTSuuPHjIckHmynKv8ejzKagpBY2b7fufceHSP0gpI3lFBx_oWQuqai5qRcBCftI3S6L1X72gl6mtKWkIYLyp6gE8qo4B0hp-j2EnQOMWFwzursxzXOG4tdiANkH0YMo8Hh3pv5FRxOU7_beGMT9oXiXej7KVuDbcoTxF_P0GMHfbLPD-cZ-nZ58XXxoVp-vLpevFtWuiEkV3alHQjaOgMtOCE50WBMvQJDKZVESgeaG9CStdA5Y1lHZCM5dcRqbeuOnaG389zdtBqs0XbMEXq1i34oLlQAr_4mo9-odbhT-5REw8uA14cBMfycins1-KRt38Now5RU0XQda-oipLNQx5BStO64hBK1z179k33pefWnu4eOQ_BF8HIWbFOJ_8hZ1xIuZcHVjH3K9v6IIf5QrWCiUe3VJ9Wx9zeL77ef1bLo2cEjDKvozdqqbZjiWH7gPy5_A0XYq6o</recordid><startdate>19540601</startdate><enddate>19540601</enddate><creator>Wheatland, A. 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Hyg</addtitle><date>1954-06-01</date><risdate>1954</risdate><volume>52</volume><issue>2</issue><spage>194</spage><epage>210</epage><pages>194-210</pages><issn>0022-1724</issn><abstract>Factors affecting the formation and destruction of sulphide in the Thames Estuary have been discussed. Measurements of oxidation-reduction potentials show that the effect of oxygen in the water on conditions in deposits of mud is limited to the surface layer. The rate of formation of sulphide increases with temperature, doubling approximately for each 10° C. rise. Reduction of sulphate to sulphide will occur at temperatures as low as 5° C., but even at 25° C. is inhibited by traces of dissolved oxygen. Mud in suspension in the estuary can produce as much sulphide as compact layers of similar mud which might be more anaerobic. Oxidation of sulphide in the Thames Estuary is shown to be of a purely chemical nature; the rate of oxidation, when oxygen is present, is increased by the presence of suspended matter and iron. In the Thames Estuary, however, the rate is limited by the rate at which oxygen enters the water. Much of the experimental work described in this paper was carried out by Miss A. Laird, Mr A. E. Sutton and Mr R. B. Peel of this Laboratory. The paper is published by permission of the Department of Scientific and Industrial Research.</abstract><cop>Cambridge, UK</cop><pub>Cambridge University Press</pub><pmid>13174800</pmid><doi>10.1017/S0022172400027406</doi><tpages>17</tpages><oa>free_for_read</oa></addata></record> |
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source | JSTOR Archival Journals and Primary Sources Collection; PubMed Central; Cambridge University Press:JISC Collections:Full Collection Digital Archives (STM and HSS) (218 titles) |
subjects | Bottles Environmental Pollution Estuaries Hazardous Substances Hydrogen Mud Old Medline Oxidation Oxidation-Reduction Oxygen River water Sea water Sewage Sulfate reducing bacteria Sulfides Water Supply |
title | Factors affecting the formation and oxidation of sulphides in a polluted estuary |
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