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Type: | Resource | |
Storage: | The size of this resource is 130.5 KB | |
Created: | Oct 10, 2019 at 2:16 a.m. | |
Last updated: | Mar 28, 2020 at 6:21 p.m. (Metadata update) | |
Published date: | Oct 10, 2019 at 2:42 a.m. | |
DOI: | 10.4211/hs.5527ff2d53494455b9a9121158c02dbe | |
Citation: | See how to cite this resource |
Sharing Status: | Published |
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Views: | 1274 |
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Abstract
Biannual hydrogeologic cycle characterization in a natural semi arid environment, we have applied and compared Craig-Gordon isotopic model with the Penman physical evaporation model. Results presented include rain water, atmospheric water vapor, agricultural pool water, isotopic evaporation loss and Penman evaporation estimation Physical and isotopic methodologies are difficult to relate due to basic fundamentals and development conceptualizations. Further work is required to enhance the Craig-Gordon and Gonfiantini evaporation model and its relationship with physical methodologies to obtain accurate estimations in evaporation in natural semiarid environments.
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This resource has been replaced by a newer version | levresse, g. (2020). San juan del rio basin hydrochemistry, HydroShare, http://www.hydroshare.org/resource/27d407bdfd9e4a479b67c5f385a8e4a1 |
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Funding Agencies
This resource was created using funding from the following sources:
Agency Name | Award Title | Award Number |
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CONACYT | Characterization of the hydrothermales impacts on overexploited aquífer. | CB-255070 |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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