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Nizou, Jean; Demory, François (2015): Magnetic parameters of the Bay of Seine seafloor dried grab samples at t0 (i.e. from June to September 2011), t1 (i.e. in March 2013), t2 (i.e. in June 2013) and t3 (i.e. in September 2013) [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.830268, In supplement to: Nizou, Jean; Demory, François; Dubrulle-Brunaud, Carole (2016): Monitoring of dredged-dumped sediment dispersal off the Bay of the Seine (northern France) using environmental magnetism. Comptes Rendus Geoscience, 348(6), 451-461, https://doi.org/10.1016/j.crte.2015.02.005

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Coverage:
Median Latitude: 49.457550 * Median Longitude: -0.107245 * South-bound Latitude: 49.417382 * West-bound Longitude: -0.162164 * North-bound Latitude: 49.496335 * East-bound Longitude: -0.023729
Event(s):
Bay_of_Seine_6 (6) * Latitude: 49.496335 * Longitude: -0.162164 * Location: Bay of Seine * Method/Device: Grab (GRAB) * Comment: WGS84
Bay_of_Seine_8 (8) * Latitude: 49.489138 * Longitude: -0.129001 * Location: Bay of Seine * Method/Device: Grab (GRAB) * Comment: WGS84
Bay_of_Seine_9 (9) * Latitude: 49.491035 * Longitude: -0.058135 * Location: Bay of Seine * Method/Device: Grab (GRAB) * Comment: WGS84
Comment:
Determination of Anhysteretic Remanent Magnetization (ARM), Saturation Isothermal Remanent Magnetization (SIRM) and Isothermal Remanent Magnetization (IRM) was performed with a superconducting rock magnetometer SRM760R (2G enterprises). The ARM is an artificial magnetization gained in an alternating magnetic field of 100 mT superimposed on a steady field of 50 µT, which is comparable to the strength of the geomagnetic field. The ARM is afterward subject to demagnetization at 30 mT (ARM_30 ). The SIRM was acquired at 3 T and the IRM at 0.3 T in the opposite direction using a pulse magnetizer MMPM9 (Magnetic Measurements ltd). The S-ratio was calculated after the formula 0.5(1-IRM/SIRM) and allows for an estimation of the relative abundance of high coercivity minerals. TheS-ratio comesclose to 1when low-coercive mineralssuch a as magnetite dominate the signal,and decreaseswith increasing amount of high-coercive mineralssuch as hematite (Bloemendal et al., 1992).The Hard Isothermal Remanent Magnetization (HIRM) was calculated after the formula (SIRM-IRM)/2 and allows for an estimation of the absolute concentration of high coercivity minerals (e.g. hematite). ARM/SIRM is used as an estimator of the relative magnetic grain size. ARM_30 /ARM is also used as a magnetic grain-size estimator since samples display a constant mineralogy.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEvent
2Sample code/labelSample labelNizou, Jean
3Dry massDry mgNizou, Jeanat t0
4Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)at t0
5Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)ARM30, at t0
6Saturation isothermal remanent magnetizationSIRM10-3 A m2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9at t0
7Isothermal Remanent MagnetizationIRM10-3 Am2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9-0.3T, at t0
8Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, Jeanat t0
9Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, JeanARM30, at t0
10Saturation isothermal remanent magnetizationSIRM10-6 A m2/kgNizou, JeanSIRM3T, at t0
11Isothermal remanent magnetization, Intensity, per unit massInten IRM10-6 A*m2/kgNizou, JeanIRM-0.3T, at t0
12S-ratio (hematite/magnetite)S-rNizou, Jeanat t0
13Hard isothermal remanent magnetization, Intensity, per unit massInten HIRM10-6 A*m2/kgNizou, Jeanat t0
14ARM/ARMARM/ARMNizou, JeanARM30/ARM, at t0
15Anhysteretic remanent magnetization/saturation isothermal remanent magnetization ratioARM/SIRMNizou, Jeanat t0
16Dry massDry mgNizou, Jeanat t1
17Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)at t1
18Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)ARM30, at t1
19Saturation isothermal remanent magnetizationSIRM10-3 A m2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9SIRM3T, at t1
20Isothermal Remanent MagnetizationIRM10-3 Am2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9IRM-0.3T, at t1
21Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, Jeanat t1
22Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, JeanARM30,
23Saturation isothermal remanent magnetizationSIRM10-6 A m2/kgNizou, JeanSIRM3T, at t1
24Isothermal remanent magnetization, Intensity, per unit massInten IRM10-6 A*m2/kgNizou, JeanIRM-0.3T, at t1
25S-ratio (hematite/magnetite)S-rNizou, Jeanat t1
26Hard isothermal remanent magnetization, Intensity, per unit massInten HIRM10-6 A*m2/kgNizou, Jeanat t1
27ARM/ARMARM/ARMNizou, JeanARM30/ARM, at t1
28Anhysteretic remanent magnetization/saturation isothermal remanent magnetization ratioARM/SIRMNizou, Jeanat t1
29Dry massDry mgNizou, Jeanat t2
30Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)at t2
31Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)ARM30, at t2
32Saturation isothermal remanent magnetizationSIRM10-3 A m2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9at t2
33Isothermal Remanent MagnetizationIRM10-3 Am2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9IRM-0.3T, at t2
34Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, Jeanat t2
35Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, JeanARM30, at t2
36Saturation isothermal remanent magnetizationSIRM10-6 A m2/kgNizou, JeanSIRM3T, at t2
37Isothermal remanent magnetization, Intensity, per unit massInten IRM10-6 A*m2/kgNizou, JeanIRM-0.3T, at t2
38S-ratio (hematite/magnetite)S-rNizou, Jeanat t2
39Hard isothermal remanent magnetization, Intensity, per unit massInten HIRM10-6 A*m2/kgNizou, Jeanat t2
40ARM/ARMARM/ARMNizou, Jeanat t2
41Anhysteretic remanent magnetization/saturation isothermal remanent magnetization ratioARM/SIRMNizou, Jeanat t2
42Dry massDry mgNizou, Jeanat t3
43Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)at t3
44Anhysteretic Remanent MagnetizationARM10-3 Am2Nizou, JeanSuperconducting rock magnetometer SRM760R (2G enterprises)ARM30, at t3
45Saturation isothermal remanent magnetizationSIRM10-3 A m2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9SIRM3Tat t3
46Isothermal Remanent MagnetizationIRM10-3 Am2Nizou, JeanMagnetometer SRM760R (2G enterprises); pulse magnetizer MMPM9IRM-0.3T, at t3
47Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, Jeanat t3
48Anhysteretic remanent magnetization, Intensity, per unit massInten ARM10-6 A*m2/kgNizou, JeanARM30, at t3
49Saturation isothermal remanent magnetizationSIRM10-6 A m2/kgNizou, JeanSIRM3T, at t3
50Isothermal remanent magnetization, Intensity, per unit massInten IRM10-6 A*m2/kgNizou, JeanIRM-0.3T, at t3
51S-ratio (hematite/magnetite)S-rNizou, Jeanat t3
52Hard isothermal remanent magnetization, Intensity, per unit massInten HIRM10-6 A*m2/kgNizou, Jeanat t3
53ARM/ARMARM/ARMNizou, JeanARM30/ARM, at t3
54Anhysteretic remanent magnetization/saturation isothermal remanent magnetization ratioARM/SIRMNizou, Jeanat t3
Size:
1724 data points

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