Dissolved Organic Carbon in Groundwater Overlain by Irrigated Sugarcane.

Autor: Thayalakumaran T; Cooperative Research Centre for Irrigation Futures and CSIRO Water for a Healthy Country National Research Flagship, CSIRO Land and Water, PMB Aitkenvale, Townsville, Queensland, 4814, Australia. Thabo.Kumaran@depi.vic.gov.au.; Currently with Department of Environment and Primary Industries-Agriculture Research, 32 Lincoln Square Nth, Carlton, Vic, 3053, Australia. Thabo.Kumaran@depi.vic.gov.au., Lenahan MJ; Cooperative Research Centre for Irrigation Futures and CSIRO Water for a Healthy Country National Research Flagship, CSIRO Land and Water, PMB Aitkenvale, Townsville, Queensland, 4814, Australia. Matthew.Lenahan@aecom.com.; Currently with AECOM, PO Box 5423, Townsville, Queensland, 4810, Australia. Matthew.Lenahan@aecom.com., Bristow KL; Cooperative Research Centre for Irrigation Futures and CSIRO Water for a Healthy Country National Research Flagship, CSIRO Land and Water, PMB Aitkenvale, Townsville, Queensland, 4814, Australia.
Jazyk: angličtina
Zdroj: Ground water [Ground Water] 2015 Jul-Aug; Vol. 53 (4), pp. 525-30. Date of Electronic Publication: 2014 Sep 11.
DOI: 10.1111/gwat.12258
Abstrakt: Elevated dissolved organic carbon (DOC) has been detected in groundwater beneath irrigated sugarcane on the Burdekin coastal plain of tropical northeast Australia. The maximum value of 82 mg/L is to our knowledge the highest DOC reported for groundwater beneath irrigated cropping systems. More than half of the groundwater sampled in January 2004 (n = 46) exhibited DOC concentrations greater than 30 mg/L. DOC was progressively lower in October 2004 and January 2005, with a total decrease greater than 90% indicating varying load(s) to the aquifer. It was hypothesized that the elevated DOC found in this groundwater system is sourced at or near the soil surface and supplied to the aquifer via vertical recharge following above average rainfall. Possible sources of DOC include organic-rich sugar mill by-products applied as fertilizer and/or sugarcane sap released during harvest. CFC-12 vertical flow rates supported the hypothesis that elevated DOC (>40 mg/L) in the groundwater results from recharge events in which annual precipitation exceeds 1500 mm/year (average = 960 mm/year). Occurrence of elevated DOC concentrations, absence of electron acceptors (O2 and NO3 (-) ) and both Fe(2+) and Mn(2+) greater than 1 mg/L in shallow groundwater suggest that the DOC compounds are chemically labile. The consequence of high concentrations of labile DOC may be positive (e.g., denitrification) or negative (e.g., enhanced metal mobility and biofouling), and highlights the need to account for a wider range of water quality parameters when considering the impacts of land use on the ecology of receiving waters and/or suitability of groundwater for irrigated agriculture.
(© 2014, Commonwealth of Australia. Groundwater © 2014, National Ground Water Association.)
Databáze: MEDLINE
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