Dynamics of Dissolved Forms of Carbon and Inorganic Nitrogen in Small Watersheds of the Coastal Atlantic Forest in Southeast Brazil-Reference-Cited by-同舟云学术

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Dynamics of Dissolved Forms of Carbon and Inorganic Nitrogen in Small Watersheds of the Coastal Atlantic Forest in Southeast Brazil

Published:2010-05-07 Issue:1-4 Volume:214 Page:393-408
ISSN:0049-6979
Container-title:Water, Air, & Soil Pollution
language:en
Short-container-title:Water Air Soil Pollut

Author:

Andrade Tatiana M. B.,Camargo Plínio B.,Silva Daniela M. L.,Piccolo Marisa C.,Vieira Simone A.,Alves Luciana F.,Joly Carlos A.,Martinelli Luiz A.

Publisher

Springer Science and Business Media LLC

Subject

Pollution,Water Science and Technology,Ecological Modeling,Environmental Chemistry,Environmental Engineering

Link

http://link.springer.com/content/pdf/10.1007/s11270-010-0431-z.pdf

Reference74 articles.

1. Aber, J. D., Nadelhoffer, K. J., Steudler, P., & Mellilo, J. M. (1998). Nitrogen saturation in northern forest ecosystems: hypotheses revisited. BioScience, 48, 921–934.

2. Aitkenhead, J. A., & McDowell, W. H. (2000). Soil C:N ratio as a predictor of annual riverine DOC flux at local and global scales. Global Biogeochemical Cycle, 14, 127–138.

3. Amiotte-Suchet, P., Aubert, D., Probst, J. L., Gauthier-Lafaye, F., Probst, A., Andreux, F., et al. (1999). δ13C pattern of dissolved inorganic carbon in a small granitic catchment: the Strengbach case study (Vosges Mountains, France). Chemical Geology, 159, 129–145.

4. Asner, G. P., Seastedt, T. R., & Townsend, A. R. (1997). The decoupling of terrestrial carbon and nitrogen cycles: human influences on land cover and nitrogen supply are altering natural biogeochemical links in the biosphere. BioScience, 47, 226–234.

5. Barth, J. A. C., Cronin, A. A., Dunlop, J., & Kalin, R. M. (2003). Influence of carbonates on the riverine carbon cycle in an anthropogenically dominated catchment basin: evidence from major elements and stable carbon isotopes in the Lagan River (N. Ireland). Chemical Geology, 200, 203–216.

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