Arid
DOI10.1016/j.gexplo.2009.01.001
A groundwater isoscape (delta D, delta O-18) for Mexico
Wassenaar, L. I.1; Van Wilgenburg, S. L.2; Larson, K.3; Hobson, K. A.1
通讯作者Wassenaar, L. I.
来源期刊JOURNAL OF GEOCHEMICAL EXPLORATION
ISSN0375-6742
EISSN1879-1689
出版年2009
卷号102期号:3页码:123-136
英文摘要

Numerous studies have shown that precipitation isocapes drive delta D and delta O-18 patterns in surficial waters and in terrestrial food webs. While the GNIP (Global Network for Isotopes in Precipitation) dataset provided a key foundation for linking precipitation-terrestrial isoscapes globally, it has insufficient spatial coverage in many countries like Mexico. To overcome this limitation, we hypothesized that shallow phreatic groundwaters in Mexico could be used as an isotopic integrator of long-term seasonally weighted precipitation inputs to the landscape to aid in calibrating spatial H and 0 isotope datasets for terrestrial, biological and hydrological research. Groundwater was sampled from 234 sites in Mexico at similar to 50 km latitudinal spacing to obtain high spatial resolution and country-wide coverage for the construction of a groundwater isoscape. Our data revealed that shallow groundwater infiltration in Mexico appears largely unaffected by evaporation and reflects seasonally weighted precipitation inputs. These precipitation inputs are primarily biased to summertime when highest rainfall occurs, but a small degree of post-precipitation evaporation revealed a lower d-excess zone that corresponded to the interior semi-arid ecozone. We developed a predictive general linear model (GLM) for hydrogen and oxygen isotopic spatial patterns in Mexican groundwater and then compared the results to a validation subset of our field data, as well external data reported in the literature. The GLM used elevation, latitude, drainage basin (Atlantic vs. Pacific), and rainfall as the most relevant predictive variables. The GLM explained 81% of the overall isotopic variance observed in groundwater, 68% of the variance within our validation subset, and 77% of the variance in the external data set. Our predictive GLM is sufficiently accurate to allow for future ecological, hydrological and forensic isoscape applications in Mexico, and may be an approach that is applicable to other countries and regions where GNIP stations are lacking. Crown Copyright (C) 2009 Published by Elsevier B.V. All rights reserved.


英文关键词Isotopes Oxygen-18 Deuterium Precipitation Groundwater Mexico Isoscapes
类型Article
语种英语
国家Canada ; USA
收录类别SCI-E
WOS记录号WOS:000270251300004
WOS关键词STABLE-ISOTOPE COMPOSITION ; SURFACE WATERS ; NORTHERN MEXICO ; RESIDENCE TIME ; RIVER WATER ; PRECIPITATION ; HYDROGEN ; OXYGEN ; GEOCHEMISTRY ; GUANAJUATO
WOS类目Geochemistry & Geophysics
WOS研究方向Geochemistry & Geophysics
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/161535
作者单位1.Environm Canada, Saskatoon, SK S7N 3H5, Canada;
2.Environm Canada, Saskatoon, SK S7N 0X4, Canada;
3.Klamath Bird Observ, Ashland, OR 97520 USA
推荐引用方式
GB/T 7714
Wassenaar, L. I.,Van Wilgenburg, S. L.,Larson, K.,et al. A groundwater isoscape (delta D, delta O-18) for Mexico[J],2009,102(3):123-136.
APA Wassenaar, L. I.,Van Wilgenburg, S. L.,Larson, K.,&Hobson, K. A..(2009).A groundwater isoscape (delta D, delta O-18) for Mexico.JOURNAL OF GEOCHEMICAL EXPLORATION,102(3),123-136.
MLA Wassenaar, L. I.,et al."A groundwater isoscape (delta D, delta O-18) for Mexico".JOURNAL OF GEOCHEMICAL EXPLORATION 102.3(2009):123-136.
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