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Studies of hydrothermal processes in Crater Lake, OR Público Deposited

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https://ir.library.oregonstate.edu/concern/defaults/47429b725

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  • As a result of the past three years of field studies and our interpretation of these and other data from the literature, we conclude that there are inputs of hydrothermal fluids into the bottom of Crater Lake. The dissolved materials associated with these thermally and chemically enriched fluids, coupled with the overall hydrologic balance, control the observed chemical composition of the lake. Because the hydrothermal input dominates the flux of most dissolved chemicals into Crater Lake, the hydrothermal process is highly significant. Furthermore, the geothermal inputs have a direct effect on the density structure of the deep lake, and therefore can profoundly affect the rate of heat transport and the redistribution of dissolved salts and nutrients within the body of the lake.
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  • Master files scanned at 600 ppi (256 Grayscale, 24-bit Color) using Capture Perfect 3.0.82 on a Canon DR-9080C in TIF format. PDF derivative scanned at 300 ppi (256 B&W, 24-bit Color), using Capture Perfect 3.0.82, on a Canon DR-9080C. CVista PdfCompressor 4.0 was used for pdf compression and textual OCR.
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  • description.provenance : Made available in DSpace on 2010-03-08T23:59:24Z (GMT). No. of bitstreams: 1 StudiesHydrothermalProcessesCraterLakeOR.pdf: 10546724 bytes, checksum: 4cecfe448cc2ba538831e1a53f7ade38 (MD5) Previous issue date: 1991-05-31
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  • description.provenance : Approved for entry into archive by Linda Kathman(linda.kathman@oregonstate.edu) on 2010-03-08T23:59:24Z (GMT) No. of bitstreams: 1 StudiesHydrothermalProcessesCraterLakeOR.pdf: 10546724 bytes, checksum: 4cecfe448cc2ba538831e1a53f7ade38 (MD5)

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