Academic Journal

Isotopic discontinuities in ground water beneath Yucca Mountain

التفاصيل البيبلوغرافية
العنوان: Isotopic discontinuities in ground water beneath Yucca Mountain
المؤلفون: J S Stuckless, J F Whelan, W C Steinkampf
المساهمون: The Pennsylvania State University CiteSeerX Archives
المصدر: https://digital.library.unt.edu/ark%3A/67531/metadc618959/m2/1/high_res_d/138100.pdf.
سنة النشر: 1991
المجموعة: CiteSeerX
الوصف: Analytical data for stable isotopes in ground water from beneath Yucca Mountain, when examined in map view, show area! patterns of heterogeneity that can be interpreted in terms of mixing of at least three end members. One end member must be isotopically heavy in terms of hydrogen and oxygen and have a young apparent 14 C age such as water found at the north end of Yucca Mountain beneath Fortymile Wash. A second end member must contain isotopically heavy carbon and have an old apparent U C age such as water from the Paleozoic aquifer. The third end member cannot be tightly defined. It must be isotopically lighter than the first with respect of hydrogen and oxygen and be intermediate to the first and second end members with respect to both apparent W C age and ft i3 C. The variable isatopic compositions of hydrogen and oxygen indicate that two of the end members are waters, but the variable carbon isotopic composition could represent either a third water end member or reaction of water with a carbon-bearing solids such as caldte.
نوع الوثيقة: text
وصف الملف: application/pdf
اللغة: English
Relation: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.2661
الاتاحة: http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1045.2661
Rights: Metadata may be used without restrictions as long as the oai identifier remains attached to it.
رقم الانضمام: edsbas.67311446
قاعدة البيانات: BASE