Variable shape of magnetic hysteresis loops in the Chinese loess-paleosol sequence
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Shape of magnetic hysteresis loops of the Chinese loess-paleosol sequence is variable with low-field susceptibility and is weakly constricted in samples with intermediate susceptibility (~1.0 × 10−6 m3/kg). The analyses of the hysteresis loops show that both low- (ferrimagnetic) and high-coercivity (antiferromagnetic) components are present and the ferrimagnetic component dominate the magnetic characteristics. The ratio of ferrimagnetic over antiferromagnetic minerals (S ratio) and the superparamagnetic fraction increase with increasing susceptibility. Neither simple two-component mixtures of ferrimagnetic and antiferromagnetic minerals nor of single-domain and superparamagnetic grains fully explain the constricted hysteresis loops. We interpret the variation of the loop shape with susceptibility in the following way. When the ratio of the ferrimagnetic to antiferromagnetic contribution is relatively low (low susceptibility), the broad loop is controlled by lithogenic ferrimagnetic and antiferromagnetic minerals. For samples with intermediate susceptibility values, constricted shape originates from an addition of a broad loop from the lithogenic fraction and a narrow loop from a pedogenic fraction with high superparamagnetic content. Then with further susceptibility increase, the constricted shape almost disappears and the loop is dominated by the pedogenic fraction. The variation of hysteresis loop shape with susceptibility can be a useful indicator of the degree of pedogenesis for loess-paleosol samples.
KeywordsHysteresis Loop Magnetic Hysteresis Loop Isothermal Remanent Magnetization Chinese Loess Plateau Thermal Demagnetization
- Fine, P., K. L. Verosub, and M. J. Singer, Pedogenic and lithogenic contributions to the magnetic susceptibility record of the Chinese loess/paleosol sequence, Geophys. J. Int., 122, 97–107, 1995.Google Scholar
- Rolph, T. C., J. Shaw, E. Derbyshire, and J. T. Wang, The magnetic mineralogy of a loess section near Lanzhou, China, in The Dynamics and Environmental Context of Aeolian Sedimentary Systems, edited by K. Pye, pp. 311–323, Geological Society, London, 1993.Google Scholar
- Sasajima, S. and Y. Y. Wang, The Recent Research on Loess in China, 242 pp., Kyoto Univ. and Northwest Univ., 1984.Google Scholar
- Torii, M., L. Y. Yue, A. Hayashida, K. Maenaka, T. Yokoyama, Y. Y. Wang, and S. Sasajima, Natural remanent magnetization of loess/paleosol deposits in Luochuan area, in The Recent Research on Loess in China, edited by S. Sasajima and Y. Y. Wang, pp. 32–41, Kyoto Univ. and Northwest Univ., 1984.Google Scholar