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Ghabayen, S.; McKee, M.; Kemblowski, M. |
| Title |
Ionic and Isotopic Ratios for Identification of Salinity Sources and Missing Data in the Gaza Aquifer |
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Journal Article |
| Year |
2006 |
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Journal of Hydrology |
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318 |
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360-373 |
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THL @ christoph.kuells @ article |
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87 |
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Glavas, S.; Moschonas, N. |
| Title |
Origin of observed acidic–alkaline rains in a wet-only precipitation study in a Mediterranean coastal site, Patras, Greece |
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Journal Article |
| Year |
2002 |
Publication |
Atmospheric Environment |
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36 |
Issue |
19 |
Pages |
3089-3099 |
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Elsevier |
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THL @ luqianxue.zhang @ glavas2002origin |
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91 |
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Neal, C.; Neal, M.; Hughes, S.; Wickham, H.; Hill, L.; Harman, S. |
| Title |
Bromine and bromide in rainfall, cloud, stream and groundwater in the Plynlimon area of mid-Wales |
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Journal Article |
| Year |
2007 |
Publication |
Hydrology and Earth System Sciences |
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11 |
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1 |
Pages |
301-312 |
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THL @ christoph.kuells @ hess-11-301-2007 |
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92 |
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| Author |
Tulipano, Luigi; Fidelibus, Dolores M; Panagopoulos, Andreas (eds) |
| Title |
Groundwater management of coastal karstic aquifers |
Type |
Book Whole |
| Year |
2005 |
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EUCOST Reports |
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EU |
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Tulipano, Luigi; Fidelibus, Dolores M; Panagopoulos, Andreas |
| Language |
en |
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QS-NA-21-366-EN-R |
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92-898-0015-1 |
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THL @ christoph.kuells @ |
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93 |
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Park, H.; Schlesinger, W. |
| Title |
Global biochemical cycle of boron |
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Journal Article |
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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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