Volume 39 Issue 6
Nov.  2020
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Zhao Juxing, Li Chang'an, Huang Guangming, Jia Mingming, Lin Shuzhen, Zhang Huasong, Leng Yonghui. Grain size characteristics and origin of red earth in Yong'an, Fujian Province[J]. Bulletin of Geological Science and Technology, 2020, 39(6): 43-51. doi: 10.19509/j.cnki.dzkq.2020.0621
Citation: Zhao Juxing, Li Chang'an, Huang Guangming, Jia Mingming, Lin Shuzhen, Zhang Huasong, Leng Yonghui. Grain size characteristics and origin of red earth in Yong'an, Fujian Province[J]. Bulletin of Geological Science and Technology, 2020, 39(6): 43-51. doi: 10.19509/j.cnki.dzkq.2020.0621

Grain size characteristics and origin of red earth in Yong'an, Fujian Province

doi: 10.19509/j.cnki.dzkq.2020.0621
  • Received Date: 02 Nov 2019
  • Based on analyzing the grain size of a red earth profile in Yong'an, which is the first discovery of red earth in western Fujian province, and comparison of grain size result in Yong'an, typical eolian deposit, modern fluvial sediment and red earth in other areas, the causes of the red earth in Yong'an are discussed in this study.The results show as follows: The component particles of the red earth in Yong'an are silt predominantly, clay secondly and sand least. All the samples name clayey silt; silt and clay increase gradually and sand decreases obviously from top to bottom of the profile.The average content of 10-50 μm is 29.71%, and far less than typical atmospheric dust sediments; Sand-silt-clay triangular plot, characteristics of grain size parameter, scattergram of grain size parameter, A-M, L-M chart and frequency curves indicate the red earth in Yong'an is neither aeolian origin nor typical alluvial origin.All of the discriminant analysis results are positive value, which display the water flow action.The red earth in Yong'an is the product of intense chemical weathering after alluvial origin; The red earth of other areas in Fujian Province, Taihe in Jiangxi Province and the first terrace of Dong River in Guangdong Province have the same origin.This study has further identified the distribution of red earth in Fujian province, and origin mechanism of red earth.

     

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  • [1]
    《地质大辞典》编委会.地质大辞典[M].北京:地质出版社, 2005:321.
    [2]
    卢升高.第四纪红土的磁性与氧化铁矿物学特征及其古环境意义[J].土壤学报, 2000, 37(2):182-191.
    [3]
    胡雪峰, 沈铭能, 方圣琼.皖南网纹红土的粒度分布特征及古气候环境意义[J].第四纪研究, 2004, 24(2):160-166.
    [4]
    来红州, 莫多闻, 李新坡.洞庭盆地第四纪红土层及古气候研究[J].沉积学报, 2005, 23(1):130-137. http://d.wanfangdata.com.cn/Periodical/cjxb200501017
    [5]
    朱丽东, 叶玮, 周尚哲, 等.中亚热带第四纪红黏土的粒度特征[J].地理科学, 2006, 26(5):586-591.
    [6]
    朱丽东, 谷喜吉, 叶玮, 等.洞庭湖周边地区第四纪红土粒度特征及环境意义[J].地理科学进展, 2014, 33(1):13-22. http://www.cqvip.com/QK/96015A/201401/48410643.html
    [7]
    李保生, 温小浩, David Dian Zhang, 等.岭南粤东北地区晚第四纪红土与棕黄色沉积物的古气候转变记录[J].科学通报, 2008, 53(22):2793-2799.
    [8]
    陈秀玲, 李志忠, 靳建辉, 等.中国南方第四纪红土研究进展[J].福建师范大学学报:自然科学版, 2009, 25(5):118-124.
    [9]
    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.
    [10]
    《中国地层典》编委会.中国地层典:第四系[M].北京:地质出版社, 2000:78.
    [11]
    杨达源.中国东部的第四纪风成堆积与季风变迁[J].第四纪研究, 1991, 11(4):354-359.
    [12]
    胡雪峰, 朱煜, 沈铭能.南方网纹红土多元成因的粒度证据[J].科学通报, 2005, 50(9):917-925. http://d.wanfangdata.com.cn/Periodical/kxtb200509014
    [13]
    胡雪峰, 龚子同, 夏应菲, 等.安徽宣州黄棕色土和第四纪红土的比较研究及其古气候意义[J].土壤学报, 1999, 36(3):301-307.
    [14]
    朱显漠.中国南方的红土与红色风化壳[J].第四纪研究, 1993, 13(1):75-84. http://www.cqvip.com/Main/Detail.aspx?id=1891473
    [15]
    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.
    [16]
    Qiao Y S, Guo Z T, Hao Q Z, et al.Loess-soil sequences in southern Anhui Province:Magnetostratigraphy and paleoclimatic significance[J].Chinese Science Bulletin, 2003, 48(19):2088-2093. doi: 10.1360/03wd0183
    [17]
    Hu X F, Yuan G D, Guo Z T.Origin of Quaternary red clay of southern Anhui Province[J].Pedosphere, 1998, 8(3):267- 272.
    [18]
    Hong H L, Gu Y S, Li R B, et al.Clay mineralogy and geochemistry and their palaeoclimatic interpretation of the Pleistocene deposits in the Xuancheng section, southern China[J].Journal of Quaternary Science, 2010, 25(5):662-674. doi: 10.1002/jqs.1340
    [19]
    Hong H L, Wang C W, Zeng K F, et al.Geochemical constraints on provenance of the mid-Pleistocene red earth sediments in subtropical China[J].Sedimentary Geology, 2013, 290:97-108. doi: 10.1016/j.sedgeo.2013.03.008
    [20]
    蒋复初, 吴锡浩, 肖华国, 等.九江地区网纹红土的时代[J].地质力学学报, 1997, 3(4):27-32. http://www.cnki.com.cn/Article/CJFD1997-DZLX704.003.htm
    [21]
    李长安, 顾延生.江西修水第四系网纹红土的地层学研究[J].地层学杂志, 1997, 21(3):226-232.
    [22]
    顾延生, 李长安, 章泽军.植硅石分析在第四纪环境研究中的应用[J].地质科技情报, 1997, 16(4):55-58.
    [23]
    胡雪峰, 龚子同.江西九江泰和第四纪红土成因的比较研究[J].土壤学报, 2001, 38(1):1-9.
    [24]
    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):33-40.
    [25]
    王伟铭, 虞子冶, 杨浩.江西星子县第四纪红土层的植硅石和孢粉研究及意义[J].微体古生物学报, 1997, 14(1):41-48.
    [26]
    熊尚发, 丁仲礼, 刘东生.赣北红土与北京邻区黄土及沙漠砂的粒度特征对比[J].科学通报, 1999, 44(11):1216-1219.
    [27]
    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.
    [28]
    Xiong S F, Sun D H, Ding Z.Aeolian origin of the red earth in southeast China[J].Journal of Quaternary Science, 2002, 17(2):181-191. doi: 10.1002/jqs.663
    [29]
    Yin K, Hong H L, Gordon Jock Churchman, et al.Hydroxy-interlayered vermiculite genesis in Jiujiang Late-Pleistocene red earth sediments and significance to climate[J].Applied clayscience, 2013, 74:20-27.
    [30]
    Hu X F, Du Y, Guan C L, et al.Color variations of the Quaternary red clay in southern China and its paleoclimatic implications[J].Sedimentary Geology, 2014, 303:15-25. doi: 10.1016/j.sedgeo.2014.01.006
    [31]
    Yin K, Hong H L, Churchman G J, et al.Characterisation of the hydroxy-interlayered vermiculite from the weathering of illite in Jiujiang red earth sediments[J].Soil Research, 2014, 52(6):554. doi: 10.1071/SR14014
    [32]
    Yang L H, Zheng X M, Ye W.Sedimentary environment of vermicular red clay in South China[J].Journal of Mountain Science, 2017, 14(3):513-526. doi: 10.1007/s11629-016-3973-8
    [33]
    Yin K, Hong H L, Algeo T J, et al.Fe-oxide mineralogy of the Jiujiang red earth sediments and implications for Quaternary climate change, southern China[J].Scientific Reports, 2018, 8(1):3610. doi: 10.1038/s41598-018-20119-4
    [34]
    王春林.湖南第四系蠕虫状网纹红土的成因及其对新构造运动研究的意义[J].湖南师范大学自然科学学报, 1986, 9(1):100-106.
    [35]
    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.
    [36]
    毛龙江, 莫多闻, 杨兢红, 等.环洞庭湖地区网纹红土中稀土元素的地球化学特征[J].环境化学, 2008, 27(2):222-225.
    [37]
    Mao L J, Mo D W, Yang J H, et al.Geochemistry of trace and rare earth elements in red soils from the Dongting Lake Area and its environmental significance[J].Pedosphere, 2009, 19(5):615-622. doi: 10.1016/S1002-0160(09)60156-9
    [38]
    Lin S, Lu S G, Wang S Y.Rock magnetism, iron oxide mineralogy and geochemistry of Quaternary red earth in central China and their paleopedogenic implication[J].Palaeogeography, Palaeoclimatology, Palaeoecology, 2013, 379(3):95-103.
    [39]
    Li J Z, Tang X Q.Study on shear rate effects of reticulate red clay[J].Advanced Materials Research, 2011, 261/263:1410-1413. doi: 10.4028/www.scientific.net/AMR.261-263.1410
    [40]
    福建省第二水文工程地质队.福建省第四纪地质研究报告[R].福州: 福建省第二水文工程地质队, 1990: 3-42.
    [41]
    齐升吉, 李志忠, 陈秀玲, 等.福建东南部第四纪红土沉积粒度特征及成因分析[J].华中师范大学学报:自然科学版, 2010, 44(4):696-701.
    [42]
    齐升吉, 李志忠, 陈秀玲, 等.福州第四纪红土沉积的粒度特征及环境意义[J].湖南师范大学自然科学学报, 2011, 34(4):88-94.
    [43]
    方红, 陈秀玲, 李志忠, 等.福建北部闽江二级阶地第四纪红土粒度特征及其成因研究[J].福建师范大学学报:自然科学版, 2016, 32(5):80-85.
    [44]
    姜高磊, 刘林敬, 毕志伟, 等.河北丰宁黄土粒度特征及其环境意义[J].地质科技情报, 2018, 37(4):83-89.
    [45]
    曹宏伟, 郑祥民, 周立旻, 等.豫南黄土粒度和常量元素地球化学特征及其对物源的指示意义[J].地质科技情报, 2018, 37(6):37-45.
    [46]
    李长安, 张玉芬, 袁胜元, 等."巫山黄土"粒度特征及其对成因的指示[J].地球科学:中国地质大学学报, 2010, 35(5):879-884.
    [47]
    赖忠平, 欧先交.光释光测年基本流程[J].地理科学进展, 2013, 32(5):683-693.
    [48]
    刘东生, 安芷生, 郑洪汉.黄土与环境[M].北京:科学出版社, 1985:191-208.
    [49]
    李徐生, 杨达源, 鹿化煜.镇江下蜀黄土粒度特征及其成因初探[J].海洋地质与第四纪地质, 2001, 21(1):25-32.
    [50]
    Folk R L, Ward W C.Brazos River Bar:A study in the signification of grain size parameters[J].Journal of Sedimentary Petrology, 1957, 27:3-27. doi: 10.1306/74D70646-2B21-11D7-8648000102C1865D
    [51]
    孙东怀, 鹿化煜, David Rea, 等.中国黄土粒度的双峰分布及其古气候意义[J].沉积学报, 2000, 18(3):327-335.
    [52]
    鹿化煜, 安芷生.黄土高原红黏土与黄土古土壤粒度特征对比:红黏土风成成因的新证据[J].沉积学报, 1999, 17(2):226-232.
    [53]
    温小浩, 李保生, 郑琰明, 等.岭南东江流域一级阶地网纹红土的形成时代及其粒度特征[J].地理与地理信息科学, 2009, 25(5):59-63.
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