【24h】

A groundwater isoscape (δD, δ~(18)O) for Mexico

机译:墨西哥的地下水等值线(δD,δ〜(18)O)

获取原文
获取原文并翻译 | 示例
获取外文期刊封面目录资料

摘要

Numerous studies have shown that precipitation isocapes drive δD and δ~(18)O 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 -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.
机译:大量研究表明,降水同位素驱动表层水和陆地食物网中的δD和δ〜(18)O模式。尽管GNIP(全球降水中的同位素网络)数据集为全球链接降水-地面等值线提供了关键基础,但在墨西哥等许多国家,其空间覆盖不足。为了克服这一局限性,我们假设墨西哥的浅埋地下水可以用作长期季节性加权降水输入到景观中的同位素积分器,以帮助校准空间H和0同位素数据集,以进行陆地,生物和水文研究。在墨西哥的234个站点以-50 km的纬度间隔对地下水进行了采样,从而获得了较高的空间分辨率并在全国范围内覆盖了地下水等值线的构建。我们的数据表明,墨西哥的浅层地下水入渗似乎基本上不受蒸发的影响,并反映了季节性加权降水输入。这些降雨输入主要是在夏季出现最高降雨量时偏向夏季,但是少量的降水后蒸发显示出较低的d过量区,与内部半干旱生态区相对应。我们针对墨西哥地下水中的氢和氧同位素空间格局开发了一种预测性通用线性模型(GLM),然后将结果与我们的现场数据以及文献中报道的外部数据的验证子集进行了比较。 GLM使用海拔,纬度,流域(大西洋与太平洋)和降雨作为最相关的预测变量。 GLM解释了在地下水中观测到的总同位素变化的81%,我们的验证子集中的68%的变化以及外部数据集中77%的变化。我们的预测GLM足够准确,可以在墨西哥将来用于生态,水文和法医等值线景观,并且可能是一种适用于缺少GNIP站的其他国家和地区的方法。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号