26A study was conducted to investigate the accumulation and distribution of arsenic in 27 different fractions of rice grain (Oryza sativa L.) collected from arsenic affected area of 28Bangladesh. The agricultural soil of study area has become highly contaminated with 29 arsenic due to the excessive use of arsenic-rich underground water (0.070±0.006 mg l -1 , 30 n=6) for irrigation. Arsenic content in tissues of rice plant and in fractions of rice grain of 31 two widely cultivated rice varieties, namely BRRI dhan28 and BRRI hybrid dhan1, were 32 determined. Regardless of rice varieties, arsenic content was about 28 and 75 folds higher 33 in root than that of shoot and raw rice grain, respectively. In fractions of parboiled and 34 non-parboiled rice grain of both varieties, the order of arsenic concentrations was; rice hull 35 > bran-polish > brown rice > raw rice > polish rice. Arsenic content was higher in non-36 parboiled rice grain than that of parboiled rice.
The seasonal variations of arsenic species in lake water
were studied in the mesotrophic northern and eutrophic
southern basins of Lake Biwa in Japan. Within the
euphotic
zone, arsenite [As(III)] increased in spring and fall,
and
dimethylarsinic acid [DMAA(V)] became the dominant
form
in summer. Measurable concentrations of monomethylarsonic acid [MMAA(V)] and trivalent methylarsenic
species
[monomethylarsonous acid, MMAA(III), and
dimethylarsinous acid, DMAA(III)] also appeared,
although
they were always minor fractions. The total arsenic
concentration in the euphotic zones remained constant in
the northern basin throughout the year. However, it
was
increased by 2−4 times in the southern basin in summer.
The
enhancement was caused by the increase of As(V),
which
was accompanied by the increase of iron, manganese,
and phosphorus. The concentration of methylarsenicals
per
chlorophyll a was lower in the southern basin.
These
results indicate that the variations of arsenic species in
lake
water largely depend on biological processes, such as
the metabolism of phytoplankton, decomposition of organic
matter by bacteria, and microbial reduction of iron and
manganese oxides in sediments. Moreover, they show
that
eutrophication affects the concentration and speciation
of arsenic in the lake water.
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