Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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
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ISSN | 0375-6742 |
EISSN | 1879-1689 |
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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