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MIT research points to carbon in man-made ponds as catalyst for arsenic contamination in Bangladeshi drinking water

November 16, 2009

By Denise Brehm
Civil & Environmental Engineering

Researchers in MIT's Department of Civil and Environmental Engineering believe they have pinpointed a pathway by which arsenic may be contaminating the drinking water in Bangladesh, a phenomenon that has puzzled scientists, world health agencies and the Bangladeshi government for nearly 30 years. The research suggests that human alteration to the landscape, the construction of villages with ponds, and the adoption of irrigated agriculture are responsible for the current pattern of arsenic concentration underground. The findings also indicate that drinking-water wells drilled to a greater depth would likely provide clean water.

Bangladesh is the seventh most populous country in the world, and tens of millions of its citizens have been exposed to arsenic in their water over the past several decades. As many as 3,000 Bangladeshis die from arsenic-induced cancer each year and today approximately 2 million people in the country live with arsenic poisoning, which manifests as skin lesions and neurological disorders, and causes cardiovascular and pulmonary diseases and cancer. Allan H. Smith a professor of epidemiology at the University of California, Berkeley, calls it “the largest mass poisoning of a population in history.”

This pervasive incidence of arsenic poisoning and its link to drinking water were first identified in the early 1980s. This was not long after the population began switching from surface water sources like rivers to groundwater from tube wells — part of a national effort to decrease the incidence of bacterial illnesses caused by contaminated drinking water. But most of the tube wells have been drilled to less than 100 feet, where they draw water directly from the arsenic-contaminated shallow aquifer. Scientists have struggled to understand how the arsenic, which is naturally occurring in the underground sediment of the Ganges Delta, is getting into the groundwater.

By 2002, a research team led by Charles Harvey, the Doherty Associate Professor of Civil and Environmental Engineering at MIT, had determined that microbial metabolism of organic carbon was mobilizing the arsenic off the soils and sediments, and that crop irrigation was almost certainly playing a role in the process. But the exact sources of the contaminated water have remained elusive, until now.

In a paper appearing online in Nature Geoscience Nov. 15, Harvey, former graduate students Rebecca Neumann and Khandaker Ashfaque and co-authors explain that ponds excavated for the purpose of providing soil to build up villages for flood protection are the source of the organic carbon that presently mobilizes the arsenic in their 6-square-mile test site. The carbon settles to the bottom of the ponds, then seeps underground where microbes metabolize it. This creates the chemical conditions that cause arsenic to dissolve off the sediments and soils and into the groundwater.

The researchers also found that in their test area, which is flooded by annual monsoons, the rice fields irrigated with arsenic-laden water actually serve to filter out much of the arsenic from the water system.

"Our research shows that water from the ponds carries degradable organic carbon into the shallow aquifer. Groundwater flow, drawn by irrigation pumping, transports that pond water to the depth where dissolved arsenic concentrations are greatest and where it is then pumped up into the irrigation and drinking wells," says Harvey. "The other interesting thing we found is that the rice fields are a sink of arsenic — more arsenic goes in with the irrigation water than comes out in the groundwater."

Scott Fendorf, a professor at Stanford University who studies arsenic content in soils and sediments along the Mekong River in Cambodia, says Harvey's previous research, published in 2002, "transformed the scientific community's outlook on the problem." The current work, he adds, has two big ramifications: "It shows that human modifications are impacting the arsenic content in the groundwater; and that while the rice cropping system appears to be buffering the arsenic, the ponds excavated to provide fill to build up the villages are having a negative impact on the release of arsenic."
Intensive fieldwork

Neumann, now a postdoctoral associate at Harvard University, took seven trips and spent nearly a year doing fieldwork in Bangladesh, studying the hydrologic behavior and chemical nature of rice fields and ponds, and performing tests on rice field and pond waters to determine if the organic carbon in these water bodies would stimulate arsenic mobilization. She and Ashfaque developed an understanding of the surface and underground water flow patterns over a seven-year period, using natural tracers and a 3-D model to track rice field and pond water as it traveled into and through the subsurface.

“We extensively studied the water in about 50 irrigation wells, in 40 to 50 drinking water wells, and also in 80 monitoring wells including seven injection wells we created specifically for testing purposes,” says Ashfaque, who spent two months a year in Bangladesh from 2001-2006 overseeing installation of the team’s test wells, performing injection and pumping experiments, and testing the wells’ water. He also developed the 3-D numerical model of the site’s hydrogeological structure.

"When we compared the chemical signatures of the different water sources in our study area to the signatures of the aquifer water, we saw that water with high arsenic content originates from the human-built ponds, and water with lower arsenic content originates from the rice fields," says Neumann. "It's likely that these same processes are occurring at other sites, and it suggests that the problem could be alleviated by digging deeper drinking water wells below the influence of the ponds or by locating shallow drinking wells under rice fields." The researchers suggest that irrigation wells remain at the shallow level.
Finding a solution

Holly Michael, a professor at the University of Delaware and former PhD student in the Harvey Lab, also studies the physics of groundwater flow and transport of the dissolved arsenic in Bangladesh, but in the deeper aquifer. "My team found that if only the drinking-water wells are put into the deep, low-arsenic parts of the aquifer — at depths greater than 450 feet — then it is likely that the supply of low-arsenic water will continue for a very long time over much of the arsenic-affected area,” says Michael. "Because so much more water is pumped for irrigation, it is important that irrigation wells are not installed deeper, as this would likely cause high-arsenic groundwater to flow downward toward the wells."

Harvey and a team of environmental scientists and physicians are making plans for a multi-year study that would provide deep wells for two villages in Bangladesh whose inhabitants suffer from arsenic poisoning. There they would combine continual testing of the well water and hydrogeological modeling of the groundwater system with a study of how the clean water effects the villagers' health, placing special emphasis on the neurological development of children.

"There are all sorts of studies to show how arsenic hurts people. We're trying to turn it around and show how removal of the arsenic will help them," says Harvey.

Other co-authors on the paper are graduate student Julie Shoemaker, who helped with fieldwork, sample analysis and data synthesis, and A.B.M. Badruzzaman and M. Ashraf Ali of the Bangladesh University of Engineering and Technology, who provided logistical support for the field site in the Munshiganj district of Bangladesh.

The research was funded by the Division of Earth Sciences of the National Science Foundation and the Center for Environmental Sensing and Modeling of the Singapore-MIT Alliance for Research and Technology.

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Article abstract

Nature Geoscience
Published online: 15 November 2009 | doi:10.1038/ngeo685

Anthropogenic influences on groundwater arsenic concentrations in Bangladesh

Rebecca B. Neumann1, Khandaker N. Ashfaque1, A. B. M. Badruzzaman2, M. Ashraf Ali2, Julie K. Shoemaker3 & Charles F. Harvey1

Abstract

The origin of dissolved arsenic in the Ganges Delta has puzzled researchers ever since the report of widespread arsenic poisoning two decades ago. Today, microbially mediated oxidation of organic carbon is thought to drive the geochemical transformations that release arsenic from sediments, but the source of the organic carbon that fuels these processes remains controversial. At a typical site in Bangladesh, where groundwater-irrigated rice fields and constructed ponds are the main sources of groundwater recharge, we combine hydrologic and biogeochemical analyses to trace the origin of contaminated groundwater. Incubation experiments indicate that recharge from ponds contains biologically degradable organic carbon, whereas recharge from rice fields contains mainly recalcitrant organic carbon. Chemical and isotopic indicators as well as groundwater simulations suggest that recharge from ponds carries this degradable organic carbon into the shallow aquifer, and that groundwater flow, drawn by irrigation pumping, transports pond water to the depth where dissolved arsenic concentrations are greatest. Results also indicate that arsenic concentrations are low in groundwater originating from rice fields. Furthermore, solute composition in arsenic-contaminated water is consistent with that predicted using geochemical models of pond-water–aquifer-sediment interactions. We therefore suggest that the construction of ponds has influenced aquifer biogeochemistry, and that patterns of arsenic contamination in the shallow aquifer result from variations in the source of water, and the complex three-dimensional patterns of groundwater flow.
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1. Parsons Laboratory, Department of Civil and Environmental Engineering, Massachusetts Institute of Technology, Cambridge, Massachusetts 02139, USA
2. Department of Civil and Environmental Engineering, Bangladesh University of Engineering and Technology, Dhaka 1000, Bangladesh
3. Department of Earth and Planetary Sciences and Department of Organismic and Evolutionary Biology, Harvard University, Cambridge, Massachusetts 02138, USA

Correspondence to: Charles F. Harvey1 e-mail: charvey@mit.edu

 

 
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