| Records |
| Author |
Webster*, R.; . Oliver, M.A. |
Title  |
Geostatistics for Environmental Scientists |
Type |
Book Whole |
| Year |
2007 |
Publication |
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Chichester ; Hoboken, NJ : Wiley |
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Series Title |
Statistics in practice. |
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ISBN |
978-0-470-51726-0 |
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Approved |
no |
| Call Number |
CUT @ phaedon.kyriakidis @ Webster2007 |
Serial |
166 |
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| Author |
Goovaerts*, P. |
| Title |
Geostatistics for natural resources evaluation |
Type |
Book Whole |
| Year |
1997 |
Publication |
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| Publisher |
Oxford University Press |
Place of Publication |
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Series Title |
Applied geostatistics series |
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ISBN |
9780195115383 |
Medium |
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Approved |
no |
| Call Number |
CUT @ phaedon.kyriakidis @ Goovaerts1997 |
Serial |
168 |
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| Author |
Chilès*, J.P.; Delfiner, P. |
| Title |
Geostatistics: Modeling spatial uncertainty |
Type |
Book Whole |
| Year |
2009 |
Publication |
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Wiley |
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Series Title |
Wiley Series inWiley Series in Probability and Statistics |
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ISBN |
9780470317839 |
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no |
| Call Number |
CUT @ phaedon.kyriakidis @ chiles2009 |
Serial |
171 |
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| Author |
Park, H.; Schlesinger, W. |
| Title |
Global biochemical cycle of boron |
Type |
Journal Article |
| Year |
2002 |
Publication |
Global Biogeochemical Cycles |
Abbreviated Journal |
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| Volume |
16 |
Issue |
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Pages |
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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no |
| Call Number |
THL @ luqianxue.zhang @ article |
Serial |
94 |
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| Author |
Nisi, B.; Raco B.; Dotsika, E. |
| Title |
Groundwater Contamination Studies by Environmental Isotopes: A review |
Type |
Book Chapter |
| Year |
2014 |
Publication |
Environment, Energy and Climate Change I: Environmental Chemistry of Pollutants and Wastes |
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Springer-Verlag Berlin Heidelberg |
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Editor |
E. Jimenez |
| Language |
en |
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no |
| Call Number |
THL @ christoph.kuells @ |
Serial |
186 |
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