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Home ยป Biblio

Puttock A, Dungalt JA, Bol R, Dixon ER, Macleod CJ, Brazier RE. Stable carbon isotope analysis of fluvial sediment fluxes over two contrasting C4-C3 semi-arid vegetation transitions. Rapid Communications in Mass Spectrometry. 2012;26:2386-92.
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Turnbull L, Wainwright J, Brazier RE. Nitrogen and phosphorus dynamics during runoff events over a transition from grassland to shrubland in the south-western United States. Hydrological Processes. 2011;25:1-17.
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 Download: sev545_Turnbull2010_HydrologicalProcesses_N&P.pdf (3.11 MB)
Turnbull L, Wainwright J, Brazier RE. Changes in hydrology and erosion over a transition from grassland to shrubland. Hyrdrological Processes. 2010;24:393-414.
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 Download: sev546_Turnbull2010_HydrologicalProcesses_RunoffErosion.pdf (4.77 MB)
Turnbull L, Wainwright J, Brazier RE. Hydrology, erosion and nutrient transfers over a transition from semi-arid grassland to shrubland in the South-Western USA: A modelling assessment. Journal of Hydrology. 2010;388:258-72.
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 Download: sev544_Turnbull2010_JournalofHydrology_Modelling.pdf (1.16 MB)
Turnbull L, Brazier RE, Wainwright J, Dixon L, Bol R. Use of carbon isotope analysis to understand semi-arid erosion dynamics and long-term semi-arid land degradation. Rapid Communications in Mass Spectrometry. 2008;22:1697-702.
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Turnbull L, Wainwright J, Brazier RE. A conceptual framework for understanding semi-arid land degradation: Ecohydrological interactions across multiple-space and time scales. Ecohydrology. 2008;1:23-34.
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 Download: sev420_Turnbull_Ecohydrology_2008.pdf (220.55 KB)

University of New Mexico
National Science Foundation
Copyright © 1994-2013 The University of New Mexico - This material is based upon work supported by the National Science Foundation under Grants DEB#9634135 (3/15/97 - 2/29/04), DEB#0236154 (3/1/03 - 2/28/10), DEB#0832652 (5/1/09 - 4/30/15 (Core funding)), DEB#0936498 (9/1/09 - 8/31/14 (ARRA funding)). Any opinions, findings, and conclusions or recommendations expressed in this material are those of the author(s) and do not necessarily reflect the views of the National Science Foundation.
 
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