/AnMtgsAbsts2009.53971 Silicate Mineral Impacts On Arsenic Accumulation in Rice.

Tuesday, November 3, 2009: 10:45 AM
Convention Center, Room 329, Third Floor

Angelia Seyfferth, Environmental Earth Systems Science, Stanford Univ., Stanford, CA and Scott Fendorf, Environmental Earth System Science, Stanford Univ., Stanford, CA
Arsenic contamination of ground waters is causing the largest mass-poisoning in human history—more than 140 million people are drinking water with hazardous levels of arsenic.  Exacerbating the threat of As from drinking water is the use of As-contaminated groundwater for rice (Oryza sativa L.) irrigation during the dry season, with concomitant food-chain transfer of As from soil and/or groundwater to humans through the ingestion of contaminated rice products (e.g. rice grains, rice milk).  It has recently been shown that As(III), the dominant form of arsenic in flooded paddy soil, is transported across rice root cells similarly to silicic acid.  Silicic acid resulting from mineral dissolution within rice paddy soils may decrease arsenic uptake into edible rice grains.  Thus, variation in soil mineralogy, and specifically the solubilty of the silicate minerals present, may have a pronounced influence on arsenic accumulation within rice.   We investigated the impact of several silica-based minerals, which vary in silica solubility, on arsenic uptake and accumulation in rice. 

Three varieties of rice were grown to maturity in an initially low-silica soil that was amended with either quartz, diatamatious earth, or silica gel and had total arsenic pore-water concentrations of 250 µg/L, typical of irrigation water in Southeastern Asia.  Throughout the experiment, pore-water chemistry was monitored using mini-Rhizon tension lysimeters.  Total arsenic in plant fractions (i.e. roots, straw, husk, grain) were determined on digested samples using conventional methods (e.g. HG-ICP).  In addition, we utlized a host of advanced (micro)spectroscopic techniques to quantify and speciate arsenic forms within various plant fractions. 

                Similarly to previous work, most of the arsenic was stored in the roots and was least in the grain. Our data indicate that as dissolved silica increased, the amount of arsenic accumulated by rice decreased, but the extent varied with plant variety.  The ratio of plant-available silica to arsenite concentrations in pore-water may prove useful to predict arsenic accumulation potential in paddy rice, and alteration of this ratio may be used to reduce arsenite uptake by rice.