Spatial distribution and temporal variability of arsenic in irrigated rice fields in Bangladesh. 2. Paddy soil

被引:161
作者
Dittmar, Jessica
Voegelin, Andreas [1 ]
Roberts, Linda C.
Hug, Stephan J.
Saha, Ganesh C.
Ali, M. Ashraf
Badruzzaman, A. Borhan M.
Kretzschmar, Ruben
机构
[1] ETH, CHN, Dept Environm Sci, Inst Biogeochem & Pollutant Dynam, CH-8092 Zurich, Switzerland
[2] Swiss Fed Inst Aquat Sci & Technol Eawag, CH-8600 Dubendorf, Switzerland
[3] Bangladesh Univ Engn & Technol, Dept Civil Engn, Dhaka 1000, Bangladesh
关键词
D O I
10.1021/es0702972
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Arsenic-rich groundwater from shallow tube wells is widely used for the irrigation of boro rice in Bangladesh and West Bengal. In the long term this may lead to the accumulation of As in paddy soils and potentially have adverse effects on rice yield and quality. In the companion article in this issue, we have shown that As input into paddy fields with irrigation water is laterally heterogeneous. To assess the potential for As accumulation in soil, we investigated the lateral and vertical distribution of As in rice field soils near Sreenagar (Munshiganj, Bangladesh) and its changes over a 1 year cycle of irrigation and monsoon flooding. At the study site, 18 paddy fields are irrigated with water from a shallow tube well containing 397 +/- 7 mu g L-1 As. The analysis of soil samples collected before irrigation in December 2004 showed that soil As concentrations in paddy fields did not depend on the length of the irrigation channel between well and field inlet. Within individual fields, however, soil As contents decreased with increasing distance to the water inlet, leading to highly variable topsoil As contents (11-35 mg kg(-1), 0-10 cm). Soil As contents after irrigation (May 2005) showed that most As input occurred close to the water inlet and that most As was retained in the top few centimeters of soil. After monsoon flooding (December 2005), topsoil As contents were again close to levels measured before irrigation. Thus, As input during irrigation was at least partly counteracted by As mobilization during monsoon flooding. However, the persisting lateral As distribution suggests net arsenic accumulation over the past 15 years. More pronounced As accumulation may occur in regions with several rice crops per year, less intense monsoon flooding, or different irrigation schemes. The high lateral and vertical heterogeneity of soil As contents must be taken into account in future studies related to As accumulation in paddy soils and potential As transfer into rice.
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页码:5967 / 5972
页数:6
相关论文
共 25 条
[1]   Arsenic uptake and accumulation in rice (Oryza sativa L.) irrigated with contaminated water [J].
Abedin, MJ ;
Cotter-Howells, J ;
Meharg, AA .
PLANT AND SOIL, 2002, 240 (02) :311-319
[2]   Arsenic accumulation and metabolism in rice (Oryza sativa L.) [J].
Abedin, MJ ;
Cresser, MS ;
Meharg, AA ;
Feldmann, J ;
Cotter-Howells, J .
ENVIRONMENTAL SCIENCE & TECHNOLOGY, 2002, 36 (05) :962-968
[3]   Assessment of arsenic contamination in soils and waters in some areas of Bangladesh [J].
Alam, MB ;
Sattar, MA .
WATER SCIENCE AND TECHNOLOGY, 2000, 42 (7-8) :185-192
[4]  
ALI MA, 2003, FATE ARSENIC ENV, P85
[5]  
[Anonymous], 2003, FATE ARSENIC ENV
[6]  
BRAMMER H, 1996, GEOGRAPHY SOILD BANG
[7]   Food chain aspects of arsenic contamination in Bangladesh: Effects on quality and productivity of rice [J].
Duxbury, JM ;
Mayer, AB ;
Lauren, JG ;
Hassan, N .
JOURNAL OF ENVIRONMENTAL SCIENCE AND HEALTH PART A-TOXIC/HAZARDOUS SUBSTANCES & ENVIRONMENTAL ENGINEERING, 2003, 38 (01) :61-69
[8]   Groundwater dynamics and arsenic contamination in Bangladesh [J].
Harvey, CF ;
Ashfaque, KN ;
Yu, W ;
Badruzzaman, ABM ;
Ali, MA ;
Oates, PM ;
Michael, HA ;
Neumann, RB ;
Beckie, R ;
Islam, S ;
Ahmed, MF .
CHEMICAL GEOLOGY, 2006, 228 (1-3) :112-136
[9]   Sequestration of As by iron plaque on the roots of three rice (Oryza sativa L.) cultivars in a low-P soil with or without P fertilizer [J].
Hu, Y ;
Li, JH ;
Zhu, YG ;
Huang, YZ ;
Hu, HQ ;
Christie, P .
ENVIRONMENTAL GEOCHEMISTRY AND HEALTH, 2005, 27 (02) :169-176
[10]  
Kinniburgh D., 2001, Final Report British Geological Survey, V2