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Conde, J.E.; Sanz Alaejos, M. |
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Selenium concentrations in natural and environmental waters |
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1997 |
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Chemical Reviews |
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97 |
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6 |
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1979-2004 |
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ACS Publications |
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THL @ luqianxue.zhang @ conde1997selenium |
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98 |
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Celle-Jeanton, H.; Travi, Y.; Loÿe-Pilot, M.-D.; Huneau, F.; Bertrand, G. |
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Rainwater chemistry at a Mediterranean inland station (Avignon, France): local contribution versus long-range supply |
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2009 |
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Atmospheric Research |
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91 |
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1 |
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118-126 |
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Elsevier |
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0169-8095 |
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THL @ luqianxue.zhang @ Celle-Jeanton2009 |
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55 |
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Bouzourra, H.; Bouhlila, R.; Elango, L.; Slama, F.; Ouslati, N. |
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Characterization of mechanisms and processes of groundwater salinization in irrigated coastal area using statistics, GIS, and hydrogeochemical investigations |
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2015 |
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Environmental Science and Pollution Research |
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22 |
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4 |
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2643-2660 |
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THL @ luqianxue.zhang @ bouzourra2015characterization |
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78 |
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Bailey, R.T. |
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Title |
Selenium contamination, fate, and reactive transport in groundwater in relation to human health |
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2017 |
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Hydrogeology Journal |
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25 |
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4 |
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1191-1217 |
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THL @ luqianxue.zhang @ bailey2017selenium |
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77 |
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Park, H.; Schlesinger, W. |
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Title |
Global biochemical cycle of boron |
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2002 |
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Global Biogeochemical Cycles |
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16 |
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1072 |
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Abstract |
The global Boron (B) cycle is primarily driven by a large flux (1.44 Tg B/yr) through the atmosphere derived from seasalt aerosols. Other significant sources of atmospheric boron include emissions during the combustion of biomass (0.26-0.43 Tg B/yr) and coal, which adds 0.20 Tg B/yr as an anthropogenic contribution. These known inputs to the atmosphere cannot account for the boron removed from the atmosphere during rainfall (3.0 Tg B/yr) and estimated dry deposition (1.3-2.7 Tg B/yr). In addition to atmospheric deposition, rock weathering is a source of boron (0.19 Tg B/yr) for terrestrial ecosystems, and humans mine about 0.31 Tg B/yr from the Earth's crust. More than 4.8 Tg B/yr circulates in the biogeochemical cycle of land plants, and about 0.53-0.63 Tg B/yr is carried from land to sea by rivers. The biogeochemical cycle of boron in the sea includes 4.4 Tg B/yr circulating in the marine biosphere, and an annual loss of 0.47 Tg B/yr to the oceanic crust via a variety of sedimentary processes that collectively remove only a small fraction of the total annual inputs to the oceans. Thus with our current understanding of the global biogeochemistry of B, the atmospheric budget shows outputs > inputs, while the marine compartments show inputs > outputs. Despite these uncertainties, it is clear that the human perturbation of the global B cycle has more than doubled the mobilization of B from the crust and contributes significantly to the B transport in rivers. |
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THL @ luqianxue.zhang @ article |
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94 |
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