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We present spatial variations of magnetic concentration parameters including the low-field magnetic susceptibility and anhysteretic remanent magnetization (ARM).
As previously mentioned, the magnetic concentration parameters measured in 2015 were lower than the initial measurements.
Fig. 6 Relative paleointensity (RPI) curves related to three magnetic concentration parameters.
a, b Binary analysis of magnetic concentration parameters used in the RPI acquisition.
As suggested by Fig. 2, magnetic concentration parameters in the lake sediments decreased with increasing water depth (Fig. 4).
Very high and low values of magnetic concentration exist only in four samples that have been excluded.
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We also found that the magnetic concentrations of mud samples were reduced markedly during a period of storage for about 3 years.
Our measurements of the magnetic susceptibility and ARM of dredged sediment samples from Lake Ogawara showed that medium sand samples at shallow littoral sites are characterized by high magnetic concentrations.
Using response surface methodology and Box-Behnken design, the variables such as magnetic nanoparticle concentration, glutaraldehyde concentration, enzyme concentration, and cross linking time were optimized.
The magnetic-concentration-sensitive parameters, ARM and k, are often used to normalize the NRM for constructing paleointensity proxies (e.g., Valet 2003; Suganuma et al. 2008, 2009).
The three magnetic-concentration-sensitive parameters, magnetic susceptibility (χ or K m), ARM, and SIRM, are often used to normalize the NRM for constructing paleomagnetic paleointensity proxies (King et al. 1983; Tauxe 1993; Valet 2003).
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