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- W2044152198 abstract "Recent measurements of non-linear temperature profiles have led to the suggestion that vertical pore water advection is present in deep sea sediments in some areas. This paper examines the basis for this hypothesis and considers a number of alternative mechanisms which, even in the absence of fluid advection, may give rise to non-linear temperature profiles. These include changes in bottom water temperature, the effects of rapid deposition or removal of sediment and the release or absorption of heat by mechanical and chemical changes within the sediment column. The downwarping of sediment layers caused by the penetration of a probe is almost certain to cause a small temperature non-linearity which must define a minimum threshold below which natural curvature cannot be confidently detected. The influence of irregular topography may also be an important source of error. Stringent criteria must be applied to site selection and data interpretation if sediment temperature profiles are to yield meaningful estimates of pore water advection velocities." @default.
- W2044152198 created "2016-06-24" @default.
- W2044152198 creator A5007324504 @default.
- W2044152198 date "1984-03-01" @default.
- W2044152198 modified "2023-10-17" @default.
- W2044152198 title "Origins and significance of non-linear temperature profiles in deep-sea sediments" @default.
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- W2044152198 doi "https://doi.org/10.1111/j.1365-246x.1984.tb01916.x" @default.
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