[1] 刘东生. 中国的黄土堆积[M]. 北京:科学出版社,1965.

Liu Tungsheng. The loess deposits in China[M]. Beijing: Science Press, 1965.
[2] 郭正堂,魏兰英,吕厚远,等. 晚第四纪风尘物质成分的变化及其环境意义[J]. 第四纪研究,1999,19(1):41-48.

Guo Zhengtang, Wei Lanying, Houyuan Lü, et al. Changes in the composition of Late Pleistocene aeolian dust and the environmental significance[J]. Quaternary Sciences, 1999, 19(1): 41-48.
[3] 熊尚发,丁仲礼,刘东生. 南方红土网纹:古森林植物根系的土壤学证据[J]. 科学通报,2000,45(12):1317-1321.

Xiong Shangfa, Ding Zhongli, Liu Tungsheng. The worm-shaped veins in the red earth of South China-Pedological evidence for root traces of past forest[J]. Chinese Science Bulletin, 2000, 45(12): 1317-1321.
[4] 赵其国,杨浩. 中国南方红土与第四纪环境变迁的初步研究[J]. 第四纪研究,1995,15(2):107-116.

Zhao Qiguo, Yang Hao. A preliminary study on red earth and changes of Quaternary environment in South China[J]. Quaternary Sciences, 1995, 15(2): 107-116.
[5] 胡雪峰,程天凡,巫和昕. 南方网纹红土内是否可能存在多个“沉积—成土”过程的旋回?[J]. 科学通报,2003,48(9):969-975.

Hu Xuefeng, Cheng Tianfan, Wu Hexin. Do multiple cycles of aeolian deposit- pedogenesis exist in the reticulate red clay sections in southern China?[J]. Chinese Science Bulletin, 2003, 48(9): 969-975.
[6] 谢树成,易轶,刘育燕,等. 中国南方更新世网纹红土对全球气候变化的响应:分子化石记录[J]. 中国科学(D辑):地球科学,2003,33(5):411-417.

Xie Shucheng, Yi Yi, Liu Yuyan, et al. The Pleistocene vermicular red earth in South China signaling the global climatic change: The molecular fossil record[J]. Science China (Seri. D): Earth Sciences, 2003, 33(5): 411-417.
[7] 朱景郊. 网纹红土的成因及其研究意义[J]. 地理研究,1988,7(4):12-20.

Zhu Jingjiao. Genesis and research significance of the plinthitic horizon[J]. Geographical Research, 1988, 7(4): 12-20.
[8] 杨达源,韩辉友,周旅复,等. 安徽宣城地区中晚更新世风成堆积与环境变迁[J]. 海洋地质与第四纪地质,1991,11(2):97-104.

Yang Dayuan, Han Huiyou, Zhou Lüfu, et al. Eolian deposit and environmental change of Middle-Late Pleistocene in Xuancheng, Anhui province south of the lower reaches of the Changjiang River[J]. Marine Geology & Quaternary Geology, 1991, 11(2): 97-104.
[9] 李徐生,杨达源,鹿化煜. 皖南风尘堆积序列氧化物地球化学特征与古气候记录[J]. 海洋地质与第四纪地质,1999,19(4):75-82.

Li Xusheng, Yang Dayuan, Lu Huayu. Oxide-geochemistry features and paleocli matic record of the aeolian-dust deposi tional sequence in southern Anhui[J]. Marine Geology & Quaternary Geology, 1999, 19(4): 75-82.
[10] 刘良梧,龚子同. 宣城第四纪红色黏土剖面的发育特征[J]. 第四纪研究,2000,20(5):464-468.

Liu Liangwu, Gong Zitong. Characteristics of development of Quaternary red clay in Xuancheng, Anhui province[J]. Quaternary Sciences, 2000, 20(5): 464-468.
[11] 朱诚. 对庐山东麓第四纪沉积物物源及新构造运动的新认识[J]. 地理学报,1995,50(1):41-50.

Zhu Cheng. The new recognitions to genesis Quaternary sediments and Neotectonics in the east piedmont of the Lushan mountain[J]. Acta Geographica Sinica, 1995, 50(1): 41-50.
[12] Hu X F, Wei J, Xu L F, et al. Magnetic susceptibility of the Quaternary red clay in subtropical China and its paleoenvironmental implications[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2009, 279(3/4): 216-232.
[13] 洪祎君. 中国南方网纹红土的形成机制及网纹成熟度研究[D]. 南昌:江西师范大学,2015.

Hong Yijun. Research on the formation mechanism of reticulated red clay and growth of reticulated mottles[D]. Nanchang: Jiangxi Normal University, 2015.
[14] 胡雪峰,沈铭能,方圣琼. 皖南网纹红土的粒度分布特征及古环境意义[J]. 第四纪研究,2004,24(2):160-166.

Hu Xuefeng, Shen Mingneng, Fang Shengqiong. Grain-size distribution of the reticulate red clay in southern Anhui province and its paleo-environmental significance[J]. Quaternary Sciences, 2004, 24(2): 160-166.
[15] 黄镇国,张伟强. 中国红土期气候期构造期的耦合[J]. 地理学报,2000,55(2):200-208.

Huang Zhenguo, Zhang Weiqiang. Coupling relationship between the red earth evolution, climate change and tectonic movement in China[J]. Acta Geographica Sinica, 2000, 55(2): 200-208.
[16] 尹秋珍,郭正堂. 中国南方的网纹红土与东亚季风的异常强盛期[J]. 科学通报,2006,51(2):186-193.

Yin Qiuzhen, Guo Zhengtang. Mid-Pleistocene vermiculated red soils in southern China as an indication of unusually strengthened East Asian monsoon[J]. Chinese Science Bulletin, 2006, 51(2): 186-193.
[17] 朱照宇,吴翼,邱世藩,等. 华南沿海第四纪类网纹红土的赋存层位及其年代问题[J]. 地球科学进展,2010,25(4):391-399.

Zhu Zhaoyu, Wu Yi, Qiu Shifan, et al. The problems of stratigraphy and chronology of like-vermicular red earth formed in the Quaternary along the coast of South China[J]. Advances in Earth Science, 2010, 25(4): 391-399.
[18] 刘彩彩,邓成龙. 南方红土磁性地层年代学研究进展[J]. 地学前缘,2011,18(4):158-170.

Liu Caicai, Deng Chenglong. Magnetostratigraphy of the red soil sequences in southern China: Recent developments[J]. Earth Science Frontiers, 2011, 18(4): 158-170.
[19] 朱丽东,刘名瑜,谷喜吉,等. 金衢盆地网纹红土色度及其环境意义[J]. 海洋地质与第四纪地质,2014,34(3):133-141.

Zhu Lidong, Liu Mingyu, Gu Xiji, et al. Envionmental implication of the color index of the plinthitic red earth in Jinhua-Quzhou Basin[J]. Marine Geology & Quaternary Geology, 2014, 34(3): 133-141.
[20] 熊平生. 江西赣南地区网纹红土粒度组合特征及其指示意义[J]. 地球与环境,2011,39(4):485-491.

Xiong Pingsheng, Grain-size features of the red earth in southern Jiangxi province and its environmental significance[J]. Earth and Environment, 2011, 39(4): 485-491.
[21] 刘彩彩,邓成龙. 南方红土的磁性矿物组成及其区域性差异[J]. 第四纪研究,2012,32(4):626-634.

Liu Caicai, Deng Chenglong. Magnetic mineralogy of the red soil sequences in southern China and its variety[J]. Quaternary Sciences, 2012, 32(4): 626-634.
[22] 殷科,洪汉烈,韩文,等. 网纹红土中铁矿物与黏土矿物赋存关系的X射线衍射证据[J]. 光谱学与光谱分析,2013,33(4):1126-1129.

Yin Ke, Hong Hanlie, Han Wen, et al. Occurrence relationship between iron minerals and clay minerals in net-like red soils: Evidence from X-Ray diffraction[J]. Spectroscopy and Spectral Analysis, 2013, 33(4): 1126-1129.
[23] 叶玮,杨立辉,朱丽东,等. 中亚热带网纹红土的稀土元素特征与成因分析[J]. 地理科学,2008,28(1):40-44.

Ye Wei, Yang Lihui, Zhu Lidong, et al. Characteristics and origin of rare earth elements of vermicular red earth in middle sub-tropic zone[J]. Scientia Geographica Sinica, 2008, 28(1): 40-44.
[24] 尹秋珍,郭正堂,方小敏. 海南砖红壤的微形态特征以及南方网纹红土与砖红壤环境意义的差异[J]. 土壤学报,2006,43(3):353-361.

Yin Qiuzhen, Guo Zhengtang, Fang Xiaomin. Micromorphology of latosols in Hainan and differences between vemiculated red soils and latosols in environmental significance in South China[J]. Acta Pedologica Sinica, 2006, 43(3): 353-361.
[25] 李凤全,叶玮,王天阳,等. 网纹红土红色基质与白色条纹铁迁移模型[J]. 第四纪研究,2018,38(2):306-313.

Li Fengquan, Ye Wei, Wang Tianyang, et al. The model for iron migration between white reticulated mottles and red matrix[J]. Quaternary Sciences, 2018, 38(2): 306-313.
[26] Torrent J, Schwertmann U, Fechter H, et al. Quantitative relationships between soil color and hematite content[J]. Soil Science, 1983, 136(6): 354-358.
[27] Liu T, Ding Z, Yu Z. Susceptibility time series of the baoji section and the bearings on paleoclimatic periodicities in the last 2.5 Ma[J]. Quaternary International, 1993, 17(17):33⁃38.
[28] 宋扬,郝青振,葛俊逸,等. 黄土高原表土磁化率与气候要素的定量关系研究[J]. 第四纪研究,2012,32(4):679-689.

Song Yang, Hao Qingzhen, Ge Junyi, et al. Quantitative relationships between modern soil magnetic susceptibility and climatic variables of the Chinese Loess Plateau[J]. Quaternary Sciences, 2012, 32(4): 679-689.
[29] 安芷生, Porter S, Kukla G,等. 最近13万年黄土高原季风变迁的磁化率证据[J]. 科学通报,1990,35(7):529-532.

An Zhisheng, Porter S, Kukla G, et al. Magnetic susceptibility evidence of season winds changes on Loess Plateau during the late 139kyr[J]. Science Bulletin, 1990, 35(7): 529-532.
[30] 刘秀铭,刘东生, Heller F,等. 黄土频率磁化率与古气候冷暖变换[J]. 第四纪研究,1990(1):42-50.

Liu Xiuming, Liu Tungsheng, Heller F, et al. Frequency-dependent susceptibility of loess and Quaternary paleoclimate[J]. Quaternary Sciences, 1990(1): 42-50.
[31] 袁宝印,夏正楷,李保生,等. 中国南方红土年代地层学与地层划分问题[J]. 第四纪研究,2008,28(1):1-13.

Yuan Baoyin, Xia Zhengkai, Li Baosheng, et al. Chronostratigraphy and stratigraphic division of red soil in southern China[J]. Quaternary Sciences, 2008, 28(1): 1-13.
[32] 卢升高,董瑞斌,俞劲炎,等. 中国东部红土的磁性及其环境意义[J]. 地球物理学报,1999,42(6):764-771.

Lu Shenggao, Dong Ruibin, Yu Jinyan, et al. Magnetic measurement characterisation of red earth profile in eastern China and its environmental implications[J]. Chinese Journal of Geophysics, 1999, 42(6): 764-771.
[33] 胡雪峰,龚子同. 土壤磁化率:作为一种气候指标的局限性[J]. 土壤,1999(1):39-42.

Hu Xuefeng, Gong Zitong. Limitation of soil magnetic susceptibility as a climatic index[J]. Soils, 1999(1): 39-42.
[34] 邓黄月,郑祥民,杨立辉,等. 长江中下游地区第四纪红土磁学特征及其环境意义[J]. 沉积学报,2015,33(2):285-298.

Deng Huangyue, Zheng Xiangmin, Yang Lihui, et al. Magnetic properties of Quaternary red earth profile in Yangtze River valley and its paleo-environmental implications[J]. Acta Sedimentologica Sinica, 2015, 33(2): 285-298.
[35] 邓黄月,高悦,郑祥民,等. 我国南方红土岩石磁学特征及其磁化率增强机制[J]. 海洋地质与第四纪地质,2015,35(4):163-175.

Deng Huangyue, Gao Yue, Zheng Xiangmin, et al. Rock-magnetic characteristics of the red soils in southern China and the magnetism for enhancing magnetic susceptibility[J]. Marine Geology & Quaternary Geology, 2015, 35(4): 163-175.
[36] 刘育燕,林文姣,朱宗敏,等. 南方红土中的磁极倒转以及磁化率变动记录[J]. 地质科技情报,2003,22(3):33-36.

Liu Yuyan, Lin Wenjiao, Zhu Zongmin, et al. Geomagnetic polarity reversal records and susceptibility variations of the laterite in South China[J]. Geological Science and Technology Information, 2003, 22(3): 33-36.
[37] 卢升高,俞劲炎,章明奎,等. 长江中下游第四纪沉积物发育土壤磁性增强的环境磁学机制[J]. 沉积学报,2000,18(3):336-340.

Lu Shenggao, Yu Jinyan, Zhang Mingkui, et al. Environmental magnetism of magnetic enhancement for soils formed on Quaternary sediments in Yangtze River valley[J]. Acta Sedimentologica Sinica, 2000, 18(3): 336-340.
[38] 刘磊,殷科,朱宗敏,等. 九江红土的磁学特征及其环境意义[J]. 岩石矿物学杂志,2019,38(6):823-833.

Liu Lei, Yin Ke, Zhu Zongmin, et al. Magnetic characteristics and environmental significance of Jiujiang red earth[J]. Acta Petrologica et Mineralogica, 2019, 38(6): 823-833.
[39] 王思源. 中国南方红土磁学特征、起源及其与成土过程关系研究[D]. 杭州:浙江大学,2014.

Wang Siyuan. The red earth in southern China: Its magnetic characters, origins and pedogenic implication[D]. Hangzhou: Zhejiang University, 2014.
[40] 张智,凌超豪,贾玉连,等. 多重理化指标揭示的中国南方更新世网纹红土网纹化机制[J]. 地层学杂志,2020,44(1):95-103.

Zhang Zhi, Ling Chaohao, Jia Yulian, et al. Multi-physico chemical evidences for formation of Pleistocene reticulated soil and its environmental implication in South China[J]. Journal of Stratigraphy, 2020, 44(1): 95-103.
[41] McLennan S M. Weathering and global denudation[J]. The Journal of Geology, 1993, 101(2): 295-303.
[42] Harrison R J, Feinberg J M. Mineral magnetism: Providing new insights into geoscience processes[J]. Elements, 2009, 5(4): 209-215.
[43] 符超峰,宋友桂,强小科,等. 环境磁学在古气候环境研究中的回顾与展望[J]. 地球科学与环境学报,2009,31(3):312-322.

Fu Chaofeng, Song Yougui, Qiang Xiaoke, et al. Environmental magnetism and its application progress in paleoclimatic and paleoenvironmental changes[J]. Journal of Earth Sciences and Environment, 2009, 31(3): 312-322.
[44] Robinson S G. The Late Pleistocene palaeoclimatic record of North Atlantic deep-sea sediments revealed by mineral-magnetic measurements[J]. Physics of the Earth and Planetary Interiors, 1986, 42(1/2): 22-47.
[45] Evans M E, Heller F. Environmental magnetism: Principles and applications of enviromagnetics[M]. San Diego: Academic Press, 2003: 299.
[46] Deng C L, Shaw J, Liu Q S, et al. Mineral magnetic variation of the Jingbian loess/paleosol sequence in the northern Loess Plateau of China: Implications for Quaternary development of Asian aridification and cooling[J]. Earth and Planetary Science Letters, 2006, 241(1/2): 248-259.
[47] Liu C C, Deng C L, Liu Q S, et al. Mineral magnetism to probe into the nature of palaeomagnetic signals of subtropical red soil sequences in southern China[J]. Geophysical Journal International, 2010, 181(3): 1395-1410.
[48] 敖红,邓成龙. 磁性矿物的磁学鉴别方法回顾[J]. 地球物理学进展,2007,22(2):432-442.

Ao Hong, Deng Chenglong. Review in the identification of magnetic minerals[J]. Progress in Geophysics, 2007, 22(2): 432-442.
[49] Liu Q S, Deng C L, Yu Y, et al. Temperature dependence of magnetic susceptibility in an argon environment: Implications for pedogenesis of Chinese Loess/Palaeosols[J]. Geophysical Journal International, 2005, 161(1): 102-112.
[50] Deng C L, Zhu R X, Verosub K L, et al. Paleoclimatic significance of the temperature-dependent susceptibility of Holocene loess along a NW-SE transect in the Chinese Loess Plateau[J]. Geophysical Research Letters, 2000, 27(22): 3715-3718.
[51] Liu Q S, Torrent J, Morrás H, et al. Superparamagnetism of two modern soils from the northeastern Pampean region, Argentina and its paleoclimatic indications[J]. Geophysical Journal International, 2010, 183(2): 695-705.
[52] 卢升高. 中国土壤磁性与环境[M]. 北京:高等教育出版社,2003.

Lu Shenggao. Chinese soil magnetism and environment[M]. Beijing: Higher Education Press, 2003.
[53] Dearing J A, Dann R J L, Hay K, et al. Frequency-dependent susceptibility measurements of environmental materials[J]. Geophysical Journal International, 1996, 124(1): 228-240.
[54] Dearing J A. Environmental magnetic susceptibility: Using the Bartington MS2 system[M]. 2nd ed. England: Chi Publishing, 1999.
[55] King J, Banerjee S K, Marvin J, et al. A comparison of different magnetic methods for determining the relative grain size of magnetite in natural materials: Some results from lake sediments[J]. Earth and Planetary Science Letters, 1982, 59(2): 404-419.
[56] Maher B A, Taylor R M. Formation of ultrafine-grained magnetite in soils[J]. Nature, 1988, 336(6197): 368-370.
[57] 袁双. 网纹红土铁形态特征与网纹红土形成环境[D]. 金华:浙江师范大学,2010.

Yuan Shuang. Iron features and formation environment of vermicular red earth[D]. Jinhua: Zhejiang Normal University, 2010.
[58] 刘玉晶,陆晓辉,罗丹,等. 贵州喀斯特山区典型土壤氧化铁特征及其与土壤类型分异关系[J]. 土壤通报,2021,52(3):505-514.

Liu Yujing, Lu Xiaohui, Luo Dan, et al. Characteristics of iron oxides and their relationship with soil types in the karst mountainous areas of Guizhou[J]. Chinese Journal of Soil Science, 2021, 52(3): 505-514.
[59] 朱丽东,周尚哲,李凤全,等. 南方更新世红土氧化物地球化学特征[J]. 地球化学,2007,36(3):295-302.

Zhu Lidong, Zhou Shangzhe, Li Fengquan, et al. Geochemical behavior of major elements of Pleistocene red earth in South China[J]. Geochimica, 2007, 36(3): 295-302.
[60] 张晓,朱丽东,黄颖,等. 加积型网纹红土网纹化机制及形成环境[J]. 第四纪研究,2020,40(1):214-228.

Zhang Xiao, Zhu Lidong, Huang Ying, et al. The reticulated mechanism and its climatic implication of aggradation red earth[J]. Quaternary Sciences, 2020, 40(1): 214-228.
[61] 贾相岳. 黄土高原不同水热条件下黄土母质土壤矿物演化特征[D].武汉:华中农业大学,2013.

Jia Xiangyue.Mineralogy characteristics of soil evolution on the loess parent materials under different hydrothermal conditions on the Loess Plateau[D]. Wuhan: Huazhong Agricultural University, 2013.
[62] Balsam W L, Ellwood B B, Ji J F, et al. Magnetic susceptibility as a proxy for rainfall: Worldwide data from tropical and temperate climate[J]. Quaternary Science Reviews, 2011, 30(19/20): 2732-2744.
[63] 胡忠行,朱丽东,张卫国,等. 江西九庐公路红土剖面的磁学特征及其反映的风化成土作用[J]. 地球物理学报,2011,54(5):1319-1326.

Hu Zhongxing, Zhu Lidong, Zhang Weiguo, et al. Magnetic properties of red clay section along the Jiu-Lu highway at Jiujiang, Jiangxi and implications for pedogenesis[J]. Chinese Journal of Geophysics, 2011, 54(5): 1319-1326.
[64] 叶晓雯,韩志勇,李徐生,等. 网纹化对皖南红土特征剩磁的影响[J]. 南京大学学报(自然科学),2014,50(2):192-201.

Ye Xiaowen, Han Zhiyong, Li Xusheng, et al. The influence of reticulating process on characteristic remanence of red soil in southern Anhui province[J]. Journal of Nanjing University (Natural Sciences), 2014, 50(2): 192-201.
[65] 胡鹏翔,刘青松. 磁性矿物在成土过程中的生成转化机制及其气候意义[J]. 第四纪研究,2014,34(3):458-473.

Hu Pengxiang, Liu Qingsong. The production and transformation of magnetic minerals during pedogenesis and its paleoclimate significance[J]. Quaternary Sciences, 2014, 34(3): 458-473.
[66] 黄雨振,陈秀玲,吕镔,等. 福建北部闽江流域第四纪红土的磁学特征及其环境意义[J]. 山地学报,2018,36(4):527-535.

Huang Yuzhen, Chen Xiuling, Bin Lü, et al. Magnetic characteristics of Quaternary red earth sequence from the Minjiang drainage basin in northern Fujian and its environmental significance[J]. Mountain Research, 2018, 36(4): 527-535.
[67] 刘孝义,周桂琴,梁宝昌. 我国东北地区几种主要土壤磁化率[J]. 沈阳农学院学报,1982(1):7-13.

Liu Xiaoyi, Zhou Guiqin, Liang Baochang. Magnetic susceptibility of several soil in the Northeast China[J]. Journal of Shenyang Agricultural College, 1982(1): 7-13.
[68] 胡雪峰. “黄土—古土壤”序列中氧化铁和有机质对磁化率的影响[J]. 土壤学报,2004,41(1):7-12.

Hu Xuefeng. Influence of iron oxides and organic matter on magnetic susceptibility in the loess-paleosol sequence[J]. Acta Pedologica Sinica, 2004, 41(1): 7-12.
[69] Hu X F, Zhao J L, Zhang P F, et al. Fe isotopic composition of the Quaternary red clay in subtropical Southeast China: Redoxic Fe mobility and its Paleoenvironmental implications[J]. Chemical Geology, 2019, 524: 356-367.
[70] 李荣彪. 长江中下游网纹红土中氧化铁矿物相及其气候环境意义:以安徽宣城红土剖面为例[D]. 武汉:中国地质大学(武汉),2014.

Li Rongbiao. Iron oxide minerals and their palaeoclimatic significance in laterite profile in the middle to lower reaches of the Yangtze River: A case study in Xuancheng laterite profile[D]. Wuhan: China University of Geosciences (Wuhan), 2014.
[71] 朱丽东,姜永见,张明强,等. 庐山JL剖面红土磁化率特征及古环境记录[J]. 山地学报,2011,29(4):385-394.

Zhu Lidong, Jiang Yongjian, Zhang Mingqiang, et al. Characteristics of magnetic susceptibility and its paleoenvironmental records from JL red earth section, Lushan area[J]. Journal of Mountain Science, 2011, 29(4): 385-394.
[72] 魏东岚,沈俊杰,李永化. 红色风化壳地球化学特征及对古气候演变的响应:以辽南石槽剖面为例[J]. 地理科学,2018,38(2):307-313.

Wei Donglan, Shen Junjie, Li Yonghua. Geochemical characteristics of red weathering crust from shicao profile in southern Liaoning province and the response of paleoclimate evolution[J]. Scientia Geographica Sinica, 2018, 38(2): 307-313.
[73] 黄丽,洪军,谭文峰,等. 几种亚热带土壤铁锰胶膜和基质的表面化学特征[J]. 地球化学,2006,35(3):295-303.

Huang Li, Hong Jun, Tan Wenfeng, et al. Surface chemical characteristics of iron-manganese cutan and matrix in several subtropic soils in central China[J]. Geochimica, 2006, 35(3): 295-303.
[74] 韩志勇,李徐生,陈英勇,等. 矫顽力组分定量分析揭示下蜀黄土磁化率异常降低的原因[J]. 地球物理学报,2008,51(6):1835-1843.

Han Zhiyong, Li Xusheng, Chen Yingyong, et al. Quantification of magnetic coercivity components reveals the cause of anomalous decrease of magnetic susceptibility of the Xiashu loess[J]. Chinese Journal of Geophysics, 2008, 51(6): 1835-1843.
[75] 陈曦,张卫国,俞立中. 赤铁矿与磁铁矿混合比例对磁性参数的影响[J]. 地球物理学进展,2009,24(1):82-88.

Chen Xi, Zhang Weiguo, Yu Lizhong. The dependence of magnetic parameters on the mixing proportion of hematite and magnetite[J]. Progress in Geophysics, 2009, 24(1): 82-88.
[76] Schwertmann U. The effect of pedogenic environments on iron oxide minerals[M]//Stewart B A. Advances in soil science. New York: Springer, 1958.
[77] 刁桂仪,文启忠. 黄土风化成土过程中主要元素迁移序列[J]. 地质地球化学,1999,27(1):21-26.

Diao Guiyi, Wen Qizhong. The migration series of major elements during loess pedogenesis[J]. Geology-Geochemistry, 1999, 27(1): 21-26.
[78] 陈家坊. 土壤胶体中的氧化物[J]. 土壤通报,1981,18(2):44-49.

Chen Jiafang. Oxides in soil colloid [J]. Chinese Journal of Soil Science, 1981, 18(2): 44-49.
[79] 张家铭,王明光. 台湾红壤及森林土壤中之氧化铁[J]. 土壤学报,1995,32(1):14-22.

Zhang Jiaming, Wang Mingguang. Iron oxides distributed in red and forest soils of Taiwan[J]. Acta Pedologica Sinica, 1995, 32(1): 14-22.
[80] Liu C C, Dupont-Nivet G, Wang W, et al. Magnetic response to pedogenesis in aerobic soils of different weathering degree[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 567: 110240.
[81] Wang S Y, Lin S, Lu S G. Rock magnetism, iron oxide mineralogy and geochemistry of Quaternary red earth in central China and their paleopedogenic implication[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 379-380: 95-103.