Gas hydrates, pervasive in continental margin sediments, are expected to release methane in
response to ocean warming, but the geographic range of dissociation and subsequent flux of methane to
the ocean are not well constrained. Sediment column thermal models based on observed water column
warming trends offshore Washington (USA) show...
Gas hydrates, pervasive in continental margin sediments, are expected to release methane in
response to ocean warming, but the geographic range of dissociation and subsequent flux of methane to
the ocean are not well constrained. Sediment column thermal models based on observed water column
warming trends offshore Washington (USA) show...
Full Text:
, H. Paul Johnson1, Robert N. Harris2, and Una K. Miller1
1School of Oceanography, University of
Gas hydrates, pervasive in continental margin sediments, are expected to release methane in response to ocean warming, but the geographic range of dissociation and subsequent flux of methane to the ocean are not well constrained. Sediment column thermal models based on observed water column warming trends offshore Washington (USA) show...
This paper is devoted to the study of families of tangent lines
to curves in Euclidean three dimensional space by the medium of a
particular representation for lines.
First, a ring of elements called dual numbers is described,
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The derivation of coefficients for the transfer functions of maximally flat time-delay networks generally begins from an infinite
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We have investigated the gaseous structure of cyclohexane-
1,4-dione via electron diffraction. The large amplitude
motion, as suggested from spectroscopic, dipole moment
and earlier electron diffraction data was studied. The
structure was refined in two types of models: a single
"distorted boat" conformer, and a model comprised of a
superposition...