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Dissolved organic carbon (DOC) and t...

Chow, Alex Tat-Shing.

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Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California.

Record Type:	Language materials, printed : Monograph/item
Title/Author:	Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California./
Author:	Chow, Alex Tat-Shing.
Description:	207 p.
Notes:	Adviser: Dennis Rolston.
Contained By:	Dissertation Abstracts International61-07B.
Subject:	Agriculture, Soil Science. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9980487
ISBN:	0599866934

Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California.
Chow, Alex Tat-Shing.

Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California. - 207 p.

Adviser: Dennis Rolston.

Thesis (Ph.D.)--University of California, Davis, 2000.

Agricultural drainage from Delta islands is known to be a significant contributor of Dissolved Organic Carbon (DOC) that forms Trihalomethanes (THMs) when drinking water is chlorinated. The current agricultural practices create seasonal wet-dry cycles in the fields so that salinity, sodicity, temperature and moisture content of soils are varied. This study was carried out to understand the influences of the current agricultural practices on the production of DOC and THM precursors from surface and subsurface peat soil of the Sacramento-San Joaquin Delta. Both abiotic and biotic factors are examined independently in order to identify the major DOC and THM precursors production processes. Abiotic factors examined with successive batch soil to solution extraction were salinity and sodicity that affect the coagulation and dispersion of soil organic matter. Biotic factors examined with 8-week batch incubation were temperature and moisture that affect the rate of microbial decay of SOM, producing CO<sub>2</sub> and DOC.

ISBN: 0599866934Subjects--Topical Terms:

1017824
Agriculture, Soil Science.

Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California.
LDR:03352nam 2200325 a 45 001 936327
005 20110510
008 110510s2000 eng d
020 $a 0599866934
035 $a (UnM)AAI9980487
035 $a AAI9980487
040 $a UnM $c UnM
100 1 $a Chow, Alex Tat-Shing. $3 1260017
245 1 0 $a Dissolved organic carbon (DOC) and trihalomethane (THM) production of cultivated peat soil from the Sacramento - San Joaquin Delta, California.
300 $a 207 p.
500 $a Adviser: Dennis Rolston.
500 $a Source: Dissertation Abstracts International, Volume: 61-07, Section: B, page: 3486.
502 $a Thesis (Ph.D.)--University of California, Davis, 2000.
520 $a Agricultural drainage from Delta islands is known to be a significant contributor of Dissolved Organic Carbon (DOC) that forms Trihalomethanes (THMs) when drinking water is chlorinated. The current agricultural practices create seasonal wet-dry cycles in the fields so that salinity, sodicity, temperature and moisture content of soils are varied. This study was carried out to understand the influences of the current agricultural practices on the production of DOC and THM precursors from surface and subsurface peat soil of the Sacramento-San Joaquin Delta. Both abiotic and biotic factors are examined independently in order to identify the major DOC and THM precursors production processes. Abiotic factors examined with successive batch soil to solution extraction were salinity and sodicity that affect the coagulation and dispersion of soil organic matter. Biotic factors examined with 8-week batch incubation were temperature and moisture that affect the rate of microbial decay of SOM, producing CO<sub>2</sub> and DOC.
520 $a In the abiotic experiment, the results showed that the increase of the soil-water salinity decreases the amount of DOC and decreases its aromaticity. A decrease of SAR also decreases the amount of DOC and decreases its aromaticity. The results of the abiotic experiment showed that the salt accumulation of the summer irrigation is not the major production of DOC; instead, the salt accumulation may reduce the DOC leaching from the peat soil, if we consider the salt effects alone.
520 $a In the biotic experiment, the 8-week incubation experiments showed that temperature, moisture content and wet-dry cycles affect the microbial activities in soils, but only the flooded and the wet-dry cycle incubations increase the DOC concentration in the oxidized peat soil. However, the extracted DOC from the incubated peat soils showed lower STHMFP although there was increases in the concentration and SUVA.
520 $a In summary, the current agricultural practices alter the soil salinity and create the wet-dry and flooded conditions in the fields. The summer irrigation increases the soil salinity, decreases the DOC productions but increases the STHMFP. On the other hand, the wet-dry cycle in the summer and flooded conditions in the winter did produce DOC, but the STHMFP of DOC produced in these conditions decreased.
590 $a School code: 0029.
650 4 $a Agriculture, Soil Science. $3 1017824
650 4 $a Chemistry, Agricultural. $3 1021829
650 4 $a Environmental Sciences. $3 676987
690 $a 0481
690 $a 0749
690 $a 0768
710 2 0 $a University of California, Davis. $3 1018682
773 0 $t Dissertation Abstracts International $g 61-07B.
790 $a 0029
790 1 0 $a Rolston, Dennis, $e advisor
791 $a Ph.D.
792 $a 2000
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=9980487