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Frontiers of Earth Science

ISSN 2095-0195

ISSN 2095-0209(Online)

CN 11-5982/P

Postal Subscription Code 80-963

2018 Impact Factor: 1.205

Front Earth Sci Chin    0, Vol. Issue () : 259-265    https://doi.org/10.1007/s11707-009-0041-5
RESEARCH ARTICLE
Magnetic characteristics of topsoil from Xinjiang, Northwestern China, and their implications
Haitao WEI1, Dunsheng XIA1,2(), Fahu CHEN1, Ming JIN1, Haibin WANG1, Jia JIA1
1. Key Laboratory of West China’s Environmental System (Ministry of Education), Lanzhou University, Lanzhou 730000, China; 2. Key Laboratory of Desert and Desertification, Institute of Cold and Arid Regions Environmental and Engineering, Chinese Academy of Sciences, Lanzhou 730000, China
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Abstract

In this study, a set of environmental magnetic parameters (χlf, χfd%,χARM, SIRM, HIRM, SOFT and SIRM/χlf, χARM/SIRM and χARM/χlf) of 331 top-soil samples from Xinjiang Uygur Autonomous Region of China were systematically measured and the magnetic characteristics and its environmental significance were discussed. Our results indicate that the main magnetic minerals of these top-soils are single-domain magnetite. The content of magnetic minerals in top-soils from north Xinjiang is higher than that from south Xinjiang; however, the content of hard magnetic minerals is higher in the top-soils from south Xinjiang. The top-soils from Yili region contain similar magnetic minerals as that from south Xinjiang, but with much stronger magnetic SP content due to higher pedogenic processes. The differences in magnetic characteristics among top-soils from different regions of Xinjiang might reflect the differences of regional climatic factors, especially the precipitation.

Keywords environmental magnetism      top-soil      magnetic susceptibility      Xinjiang Uigur Autonomous Region     
Corresponding Author(s): XIA Dunsheng,Email:dsxia@lzu.edu.cn   
Issue Date: 05 September 2009
 Cite this article:   
Haitao WEI,Dunsheng XIA,Fahu CHEN, et al. Magnetic characteristics of topsoil from Xinjiang, Northwestern China, and their implications[J]. Front Earth Sci Chin, 0, (): 259-265.
 URL:  
https://academic.hep.com.cn/fesci/EN/10.1007/s11707-009-0041-5
https://academic.hep.com.cn/fesci/EN/Y0/V/I/259
Fig.1  Map showing the sampling sites
Fig.2  Magnetic parameters of top soil from Xinjiang
Fig.3  T-c curves and magnetic hysteresis loops of top soil from Xinjiang
North XinjiangYili ValleySouth XinjiangKumutage
maxminmeanmaxminmeanmaxminmeanmaxminmean
χlf /(10-8 m3·kg-1)1178.37 20.25 205.36 108.88 25.32 72.19 377.16 9.77 75.27 68.78 18.19 29.36
SIRM/(10-5 Am2·kg-1)10438.83 219.52 2135.60 1468.57 227.64 858.85 2817.76 127.98 780.66 1061.21 283.28 508.54
χfd%/%6.88 0.77 1.82 6.60 0.69 2.43 5.55 0.15 1.62 3.81 0.21 1.83
χARM/(10-8 m3·kg-1)776.11 57.38 243.45 421.35 43.67 152.94 212.58 24.94 78.12 147.80 31.32 75.43
HIRM/(10-5 Am2·kg-1) 181.71 13.72 60.74 76.41 10.08 40.17 154.25 4.76 42.05 53.87 13.38 27.55
SOFT/(10-5 Am2·kg-1) 2690.54 41.87 603.72 371.06 60.50 209.05 988.99 20.78 226.85 330.60 62.42 124.89
HARD%/%11.72 0.80 3.50 9.50 3.33 4.90 39.63 1.36 6.95 7.54 2.97 5.64
S-20 mT /%45.79 19.08 27.38 29.77 21.05 24.70 41.90 11.59 27.02 40.41 11.70 24.24
S-100 mT /%86.24 55.10 78.17 78.56 69.37 73.94 86.89 39.17 75.27 85.07 64.15 72.14
S-300 mT /% 99.20 88.28 96.50 96.67 90.50 95.10 98.64 60.37 93.05 97.03 92.46 94.36
SIRMχif /(103 Am-1)19.29 4.05 11.78 15.96 5.87 11.69 21.38 3.96 11.48 28.06 6.60 18.19
χARMSIRM/SIRM/(10-3 Am-1)0.50 0.07 0.14 0.49 0.10 0.19 0.15 0.08 0.12 0.19 0.12 0.15
Tab.1  Magnetic parameters of topsoil samples from Xinjiang
Fig.4  Scatter plot of magnetic parameters of top soil from Xinjiang
1 An Z S, Porter S C, Zhou W J, Lv Y C, Donahue D J, Head M J, Wu X H, Ren J Z, Zheng H B (1993). Episode of strengthened summer monsoon climate of Younger Dryas age on the Loess Plateau of central China. Quaternary Research , 39: 45-54
doi: 10.1006/qres.1993.1005
2 Aoki I, Kurosaki Y, Osada R, Sato T, Kimura F (2005). Dust storms generated by mesoscale cold fronts in the Tarim Basin, Northwest China. Geophysical Research Letters , 32: L06807
doi: 10.1029/2004GL021776
3 Chen F H, Huang X Z, Yang M L, Fan Y, Zhao H (2006). Westerly dominated holocene climate model in arid central Asia-case study on Bosten Lake, Xinjiang, China. Quaternary Sciences , 26(6): 881-887 (in Chinese with English abstract)
4 Chen F H, Yu Z C, Yang M L, Emi Ito, Wang S M, Madsen D B, Huang X Z, Zhao Y, Tomonori Sato, Birks H B, Ian Boomer, Chen J H, An C B, Wunneman B (2008). Holocene moisture evolution in arid central Asia and its out-of-phase relationship with Asian monsoon history. Quaternary Science Reviews , 27(3-4): 351-364
doi: 10.1016/j.quascirev.2007.10.017
5 Dearing J A, Bird P M, Dann R J L, Benjamin S F (1997). Secondary ferrimagnetic minerals in Welsh soils: a comparison of mineral magnetic detection methods and implications for mineral formation. Geophysical Journal International , 130(3): 727-736
doi: 10.1111/j.1365-246X.1997.tb01867.x
6 Deng C L, Liu Q S, Pan Y X, Zhu R X (2007). Environmental magnetism of Chinese loess-paleosol sequences. Quaternary Sciences , 27(2): 193-209 (in Chinese with English abstract)
7 Egli R, Lowrie W (2002). Anhysteretic remanent magnetization of fine magnetic particles. Journal of Geophysics Research , 107(B10): 2209
doi: 10.1029/2001JB000671
8 Evans M E, Heller F (2003). Environmental Magnetism. London: Academic Press, 1-293
9 Heller F, Liu T S (1984). Magnetism of Chinese loess deposits. Geophysical Journal of the Royal astronomical Society . 77(1): 125-141
10 Heller F, Liu T S (1986). Palaeoclimate and sedimentary history from magnetic susceptibility of loess in China. Geophysical Research Letters , 13(11): 1169-1172
doi: 10.1029/GL013i011p01169
11 Hu R J, Fan Z L, Wang Y J, Yang Q, Huang Y Y (2001). Assessment about the impact of climate change on environment in Xingjian since Recent 50 Years. Arid Land Geography , 24(2): 7-13 (in Chinese with English abstract)
12 Huo W, Ali Mamtimin, Liu X C, Shang H M, Qin H (2007). Correlation between years of warm winter and precipitations of spring and summer. Arid Land Geography , 30(2): 257-261 (in Chinese with English abstract)
13 Institute of geology and mineral resources, Xinjiang (2000). Atlas of paleogeography in Xinjiang. Xinjiang Geology , 18(4): 356-393 (in Chinese)
14 Kent D V (1982). Apparent correlation of paleomagnetic intensity and climatic records in deep-sea sediments. Nature , 299: 538-539
doi: 10.1038/299538a0
15 Kukla G, Heller F, Liu X M, Xu T C, Liu T S, An Z S (1988). Pleistocene climates in China dated by magnetic susceptibility. Geology , 16(9): 811-814
doi: 10.1130/0091-7613(1988)016<0811:PCICDB>2.3.CO;2
16 Lees J, Dearing J A (1999). Additional measurements using a vibrating magnetometer, In: Walden J, Oldfield F, Smith J, . Environmental Magnetism: A Practical Guide No. 6 . London: Quaternary Research Association, 185-196
17 Liu Q S, Banerjee S K, Jackson M J, Maher B A, Pan Y X, Zhu R X, Deng C L, Chen F H (2004). Grain sizes of susceptibility and anhysteretic remanent magnetization carriers in Chinese loess/paleosol sequences. Journal of Geophysical Research , 109(B3), B03101
doi: 10.1029/2003JB002747
18 Liu X (2004). Palaeogeography of the Meso-Cenozoic and crustal tectonic evolution of basin-mountain area in northwestern China. Journal of Palaeogeography , 6(4): 448-458 (in Chinese with English abstract)
19 Liu X M, An Z S, Rolph T, Qiang X K, Paul H, Lv H Y, Zhou J, Cai Y J (2001). Magnetic properties of the Tertiary red clay from Gansu Province, China and its paleoclimatic significance. Science in China , 44(7): 635-651
20 Liu X M, Xia D S, Liu T S, Ding Z L, Chen F H, Beget J E (2007). Discussion on two models of paleoclimatic records of magnetic susceptibility of Alaskan and Chinese Loess. Quaternary Sciences , 27(2): 210-220 (in Chinese with English abstract)
21 Lv H Y, Han J M, Wu N Q, Guo Z T (1994). Analysis on magnetism and paleoclimate meaning in modern soil of China. Science in China (Series B) , 24(12): 1291-1297
22 Mao W Y, Jiang Y A, Li J F (2006). Analysis on the linear tendency of precipitation in North Xinjiang. Arid Land Geography , 29(6): 797-802 (in Chinese with English abstract)
23 Porter S C, Hallet B, Wu X H, An Z S (2001). Dependence of near surface magnetic susceptibility on dust accumulation rate and precipitation on the Chinese Loess Plateau. Quaternary Research , 55(3): 271-283
doi: 10.1006/qres.2001.2224
24 Rolph T C, Shaw J, Derbyshire E, Wang J T (1993). The magnetic mineralogy of a loess section near Lanzhou, China. Geological Society Special Publication , 72: 311-323
25 Sun D H, Wu X H, Liu T S (1996). Evolution of the summer monsoon regime over the Loess Plateau of the last 150 ka. Science in China (Series.D) , 39(5): 503-511
26 Thompson R, Oldfield F (1986). Environmental Magnetism. London: Allen Unwin, 1-227
27 Thouveny N, Beaulieu J L, Bonifay E (1994). Climate variations in Europe over the past 140 kyr deduced from rock magnetism. Nature , 371: 503-506
doi: 10.1038/371503a0
28 Wang D L (2000), Paleogeography of paleoneogone in Xinjiang, Xinjiang Geology , 18(4): 352-356
29 Xia D S, Chen F H, Ma J Y, Liu X M, Zhang W G, Wang X M, Wei H T (2007). Environmental magnetic investigations of top soils along a NM-SE transect from the Chinese loess plateau of the Alxa Plateau. Quaternary Sciences , 28(6): 1001-1008 (in Chinese with English abstract)
30 Xia D S, Wei H T, Ma J Y, Wang X M, Zhang J W, Zhao H (2006). Magnetic characteristics of arid region of central Asia and their Paleoenvironmental significance. Quaternary Sciences , 26(6): 937-946 (in Chinese with English abstract)
31 Xu G Q, Wei W S (2004). Climate change of Xinjiang and its impact on eco-environment. Arid Land Geography , 27(1): 14-18 (in Chinese with English abstract)
32 Yang Q (1998). The characters of climatic changes during the last 10 years in Xinjiang. Journal of Palaeogeography , 2: 9-13 (in Chinese)
33 Ye W (2001). Study on magnetic susceptibility of loess and paleosol sequences in westerly region of Xinjiang. Journal of Desert Research , 21(4): 381-386 (in Chinese with English abstract)
34 Yu Y, Dunlop D J (2003). Decay-rate dependence of anhysteretic remanence: fundamental origin and paleo-magnetic applications. Journal of Geophysical Research , 108(B12): 2550
doi: 10.1029/2003JB002589
35 Yuan Y Y, Mu G J (2004). Features of spring climate change in Tianshan Mountainous area for the recent 40 Years and comparison with that in plain area of Xinjiang, Arid Land Geography . 27(1): 35-40 (in Chinese with English abstract)
36 Zhou L P, Oldfield F, Wintle A G, Robinson S G, Wang J T (1990). Partly pedogenic origin of magnetic variations in Chinese loess. Nature , (346): 737-739
doi: 10.1038/346737a0
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