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20240329122006.0 |
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160227s1991 dcu o 000 0 eng d |
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|a 994495217
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|a 9780309544153
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|a 0309544157
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|a DEBBG
|b BV044107598
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|a (OCoLC)940510366
|z (OCoLC)994495217
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|a n-us-nv
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|a GB1025.N4 ǂb N35 1992eb
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|a 551.49/09793/34
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|a UAMI
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|a Staff, National Research Council.
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|a Ground Water at Yucca Mountain :
|b How High Can It Rise?.
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| 260 |
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|a Washington :
|b National Academies Press,
|c 1991.
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| 300 |
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|a 1 online resource (240 pages)
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| 336 |
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|a text
|b txt
|2 rdacontent
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|a computer
|b c
|2 rdamedia
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|a online resource
|b cr
|2 rdacarrier
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|a Print version record.
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|a Ground Water at Yucca Mountain How High Can It Rise?; Copyright; Contents; Executive Summary; INTRODUCTION; HAS IT HAPPENED?; Soils; Springs; Textural/Morphologic Evidence; Breccias; Isotopes; CONCLUSION; CAN IT HAPPEN?; Increased Rainfall; Volcanic Intrusion; Earthquakes; RECOMMENDATIONS; Steep Hydraulic Gradient; Paleozoic Carbonate Aquifer; Scientific Integration/Coordination; 1-Introduction ; REFERENCES; 2-Water Levels in the Vicinity of the Proposed Repository in the Last 100,000 Years ; GEOLOGIC SETTING OF YUCCA MOUNTAIN AND ENVIRONS; Paleozoic; Mesozoic; Cenozoic; Extension.
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| 505 |
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|a Volcanic ActivityActive Tectonics; EPISODIC GROUND-WATER DISCHARGE THESIS; SOIL DEVELOPMENT AND GEOMORPHOLOGICAL CHARACTER OF THE REGION; HYDROLOGIC EVIDENCE FROM SPRINGS; Devils Hole; Wahmonie Spring; The Age of the Wahmonie Site; Cane Spring; MORPHOLOGIC/TEXTURAL EVIDENCE EXHIBITED BY CHEMICAL PRECIPITATES; EVIDENCE EXHIBITED BY BRECCIAS; GEOCHEMICAL AND MINERALOGICAL CONSIDERATIONS; ISOTOPIC EVIDENCE; Stable Isotopes: 13C and 18O; Tracer Isotopes: Sr, U, and Th; CONCLUSIONS; RECOMMENDATIONS; Additional Characterization of Carbonate Veins in Core; Fluid Inclusion Studies.
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| 505 |
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|a Isotopic Composition of Windblown DustAdditional Studies at Site 199; REFERENCES; 3-Might Increased Rainfall Cause Flooding of the Proposed Repository? ; INTRODUCTION; HYDROGEOLOGICAL SETTING; A MODEL OF GROUND-WATER FLOW AT YUCCA MOUNTAIN; EVIDENCE FOR PAST VARIABILITY IN RAINFALL; Chronological Framework; Geographic and Paleohydrologic Framework; The Paleoecological Record; PALEOCLIMATIC RECONSTRUCTIONS; Full-Glacial Climates; The Terminal Wisconsin-Early Holocene; Climates of the Last 8,000 Years; MODEL CALCULATIONS OF POTENTIAL RISE IN THE GROUND-WATER TABLE DUE TO INCREASED PRECIPITATION.
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|a CONCLUSIONSRECOMMENDATIONS; REFERENCES; 4-Can an Igneous Intrusion Raise the Water Table to the Proposed Repository Level? ; SUMMARY OF TERTIARY VOLCANIC HISTORY OF THE REGION; STYLE AND SIZE OF A LIKELY INTRUSION IN THE YUCCA MOUNTAIN REGION; MODELS OF WATER TABLE RISE ACCOMPANYING DIKE INTRUSION; POSSIBLE DEEP (LOWER CRUSTAL) MAGMA CHAMBERS IN THE YUCCA MOUNTAIN REGION; PROBABILISTIC ASSESSMENT OF THE LIKELIHOOD OF A BASALTIC DIKE INTRUSION; CONCLUSIONS; RECOMMENDATIONS; REFERENCES; 5-Could a Nearby Earthquake Cause Flooding of the Proposed Repository? ; INTRODUCTION.
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| 505 |
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|a Contemporary Crustal MotionsRecommendation; HYDROLOGIC RESPONSES TO EARTHQUAKES; HISTORICAL EVIDENCE; Loma Prieta, California; Anchorage, Alaska; Borah Peak, Idaho; RECOMMENDATION; EARTHQUAKE MODELS; Introduction; Dislocation Models; Regional Stress Change Models; Sources of Information on In Situ Physical Properties; CONCLUSIONS BASED ON RESULTS OF MODELING TO DATE; A Possible Alternate Modeling Approach: Discontinuum Analysis of Ground-Water Motion; RECOMMENDATION; EARTHQUAKE PROBABILITY; CONCLUSIONS; RECOMMENDATIONS; REFERENCES; 6-Summary of Conclusions and Recommendations.
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| 500 |
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|a Has it happened?
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| 546 |
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|a English.
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| 590 |
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|a ProQuest Ebook Central
|b Ebook Central Academic Complete
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| 650 |
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0 |
|a Groundwater
|z Nevada
|z Yucca Mountain.
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| 650 |
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0 |
|a Radioactive waste disposal in the ground
|z Nevada
|z Yucca Mountain.
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| 650 |
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6 |
|a Eau souterraine
|z Nevada
|z Yucca, Mont.
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| 650 |
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6 |
|a Déchets radioactifs
|x Élimination dans le sol
|z Nevada
|z Yucca, Mont.
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| 650 |
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7 |
|a Groundwater
|2 fast
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| 650 |
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|a Radioactive waste disposal in the ground
|2 fast
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| 651 |
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7 |
|a Nevada
|z Yucca Mountain
|2 fast
|1 https://id.oclc.org/worldcat/entity/E39PBJqFTFdkrmcJfJdTv8hfv3
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| 776 |
0 |
8 |
|i Print version:
|a Staff, National Research Council.
|t Ground Water at Yucca Mountain : How High Can It Rise?
|d Washington : National Academies Press, ©1991
|z 9780309047487
|
| 856 |
4 |
0 |
|u https://ebookcentral.uam.elogim.com/lib/uam-ebooks/detail.action?docID=3376897
|z Texto completo
|
| 938 |
|
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|a ProQuest Ebook Central
|b EBLB
|n EBL3376897
|
| 994 |
|
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|a 92
|b IZTAP
|
