Dating pelagic clay can be a challenge due to its slow sedimentation rate, post-depositional alteration, and lack of biogenic deposition. Co-based dating techniques have the potential to create age models in pelagic clay under the assumption that the flux of non-detrital Co to the seafloor is spatially and temporally constant,...
Dating pelagic clay can be a challenge due to its slow sedimentation rate, post-depositional alteration, and lack of biogenic deposition. Co-based dating techniques have the potential to create age models in pelagic clay under the assumption that the flux of non-detrital Co to the seafloor is spatially and temporally constant,...
Dating pelagic clay can be a challenge due to its slow sedimentation rate, post-depositional alteration, and lack of biogenic deposition. Co-based dating techniques have the potential to create age models in pelagic clay under the assumption that the flux of non-detrital Co to the seafloor is spatially and temporally constant,...
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Pacific Gyre
Ann G. Dunlea1, Richard W. Murray1, Justine Sauvage2, Robert A. Pockalny2, Arthur J
Dating pelagic clay can be a challenge due to its slow sedimentation rate, post-depositional alteration, and lack of biogenic deposition. Co-based dating techniques have the potential to create age models in pelagic clay under the assumption that the flux of non-detrital Co to the seafloor is spatially and temporally constant,...
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. W., Sauvage, J., Pockalny, R. A., Spivack, A. J., Harris,
R. N., & D'Hondt, S. (2015). Cobalt‐based
Temperature anomalies can identify locations of seeps of groundwater into surface waters.
However, the method’s sensitivity to details such as thermometer burial depth, sediment material, seep
velocity, and surface water current are largely unknown. We report on a series of laboratory flume experiments
in which controlled seeps under variable sediment...
Temperature anomalies can identify locations of seeps of groundwater into surface waters.
However, the method’s sensitivity to details such as thermometer burial depth, sediment material, seep
velocity, and surface water current are largely unknown. We report on a series of laboratory flume experiments
in which controlled seeps under variable sediment...
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following values results in the temperature profile shown in Figure 1:
𝑞 = 5e-7 m/s, (dashed line), 5e-6
Temperature anomalies can identify locations of seeps of groundwater into surface waters.
However, the method’s sensitivity to details such as thermometer burial depth, sediment material, seep
velocity, and surface water current are largely unknown. We report on a series of laboratory flume experiments
in which controlled seeps under variable sediment...
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Selker, F., and J. S. Selker (2014), Flume testing of underwater seep detection
using temperature
The first direct measurement of electron neutrino quasielastic and quasielasticlike scattering on hydrocarbon in the few-GeV region of incident neutrino energy has been carried out using the MINERvA detector in the NuMI beam at Fermilab. The flux-integrated differential cross sections in the electron production angle, electron energy, and Q² are...
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The first direct measurement of electron neutrino quasielastic and quasielasticlike scattering on hydrocarbon in the few-GeV region of incident neutrino energy has been carried out using the MINERvA detector in the NuMI beam at Fermilab. The flux-integrated differential cross sections in the electron production angle, electron energy, and Q² are...
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. Chvojka,1 H. da Motta,6 J. Devan,3 S. A. Dytman,7 G. A. Díaz,1,8 B. Eberly,7,† J. Felix,9
L. Fields,4,10
Error in Distributed Temperature Sensor (DTS) water temperature measurements may
be introduced by contact of the fiber optic cable sensor with bed materials (e.g.,
seafloor, lakebed, stream bed). Heat conduction from the bed materials can affect cable
temperature and the resulting DTS measurements. In the Middle Fork John Day River,...
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conduction impact on fiber optic DTS water temper-
ature measurements
T. O’Donnell Meininger and J. S