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Triki*, I.; N.Trabelsi; Zairi, M.; Dhia, H.B. |
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Multivariate statistical and geostatistical techniques for assessing groundwater salinization in Sfax, a coastal region of eastern Tunisia |
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2014 |
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Desalination Water Treat. |
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52 |
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1980-1989 |
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CUT @ phaedon.kyriakidis @ trikia2014 |
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107 |
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Emadi*, M.; Baghernejad, M. |
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Comparison of spatial interpolation techniques for mapping soil pH and salinity in agricultural coastal areas, northern Iran |
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2014 |
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Arch. Agron. Soil Sci. |
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60:9 |
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1315-1327 |
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CUT @ phaedon.kyriakidis @ Emadia2014 |
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136 |
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Varouchakis, E.A.; Theodoridou, P.G.; Karatzas, G.P. |
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Decision-making tool for groundwater level spatial distribution and risk assessment using geostatistics in R |
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2020 |
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J. Hazard. Toxic Radioact. Waste |
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24 (1) |
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04019031 |
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CUT @ phaedon.kyriakidis @ varouchakis2020 |
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106 |
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Herckenrath*, D.; Langevin, C.D.; Doherty, J. |
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Predictive uncertainty analysis of a saltwater intrusion modelusing null‐space Monte Carlo |
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2011 |
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Water Resour. Res. |
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47 |
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05504 |
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CUT @ phaedon.kyriakidis @ Herckenrath2011 |
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150 |
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Park, H.; Schlesinger, W. |
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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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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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