Citation: | YANG Lihui, YE Wei, WANG Caixia, CHEN Jing, HU Chunsheng. EFFECTS OF FINE FERROMAGNETIC NODULES ON GRAIN SIZE ANALYSIS OF QUATERNARY RED CLAY IN SOUTHERN CHINA[J]. Marine Geology & Quaternary Geology, 2016, 36(2): 161-166. DOI: 10.16562/j.cnki.0256-1492.2016.02.018 |
[1] |
朱显谟. 中国南方的红土与红色风化壳[J]. 水土保持研究, 1995, 2(4):94-101.
[ZHU Xianmo.Red clay and red weathering crust in southern China[J]. Research of Soil and Water Conservation, 1995, 2(4):94-101.]
|
[2] |
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):918-925.
[HU Xuefeng, ZHU Yu, SHEN Mingneng. The granularity evidence of multi-cause formation of vermicular red clay[J]. Chinese Science Bulletin, 2005, 50(9):918-925.]
|
[3] |
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.
[HU Xuefeng, GONG Zitong. Comparative study on the origin of Quaternary Red Earth in Jiujiang and Taihe, Jiangxi Province[J]. Acta Pedologica Sinica, 2001, 38(1):1-9.]
|
[4] |
Xiong S, Sun D, Ding Z. Aeolian origin of the red earth in southeast China[J]. Journal of Quaternary Science, 2002,17(2):181-191.
|
[5] |
李徐生, 杨达源, 鹿化煜, 等. 皖南第四纪风尘堆积序列的粒度特征及其意义[J]. 海洋地质与第四纪地质, 1999, 19(4):75-82.
[LI Xusheng, YANG Dayuan, LU Huayu,et al. Oxide-geochemistry features and paleoclimatic record of the aeolian-dust depositional sequence in southern Anhui[J]. Marine Geology and Quaternary Geology, 1999, 19(4):75-82.]
|
[6] |
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.]
|
[7] |
Xuefeng Hu, Ji Wei, Yan Du, et al. Regional distribution of the Quaternary Red Clay with aeolian dust characteristics in subtropical China and its paleoclimatic implications[J].Geoderma,2010,159(3):317-334.
|
[8] |
杨立辉, 叶玮, 郑详民, 等. 河漫滩相沉积与风成沉积粒度判别函数的建立及在红土中应用[J]. 地理研究, 2014, 33(10):1848-1856.
[YANG Lihui, YE Wei, ZHENG Xiangmin,et al. The discriminant function with grain size of floodplain and Aeolian sediments and its application in the Quaternary red clay[J]. Geographical Research, 2014, 33(10):1848-1856.]
|
[9] |
Hu X F, Jiang W, Ye W, et al.Yellow-brown earth on Quaternary red clay in Langxi County, Anhui Province in subtropical China:Evidence for paleo-climatic change in late quaternary period[J]. Journal of Plant Nutrition and Soil Science, 2008, 171(4):542-551.
|
[10] |
魏骥, 胡雪峰, 许良峰, 等. 长江中游地区第四纪红土的二元结构及古环境意义[J]. 土壤学报, 2010, 47(5):826-835.
[WEI Ji, HU Xuefeng, XU Liangfeng, et al.Dualistic structure of the Quaternary red clay in the middle reaches of the Yangtze river and its paleoenvironmental implication[J]. Pedologica Sinica, 2010, 47(5):826-835.]
|
[11] |
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):586-590.
[ZHU Lidong, YE Wei, ZHOU Shangzhe, et al. Grain-size features of red earth in mid-subtropics[J]. Geographica Sinica, 2006, 26(5):586-590.]
|
[12] |
叶玮, 朱丽东, 李凤全, 等. 中国中亚热带网纹红土的地球化学特征与沉积环境[J]. 土壤学报, 2008, 45(3):385-391.
[YE Wei, ZHU Lidong, LI Fengquan,et al. Sedimentary environment of vermicular red earth in mid-subtropical China[J]. Pedologica Sinica, 2008, 45(3):385-391.]
|
[13] |
杨立辉, 叶玮, 朱丽东, 等. 第四纪加积型红土与黄土的风成相似性探讨[J]. 干旱区地理, 2008, 31(3):341-347.
[YANG Lihui, YE Wei, ZHU Lidong, et al. The aeolian comparability of aggradational Red Earth in southern China and loess in northern China[J]. Land Geography, 2008, 31(3):341-347.]
|
[14] |
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):41-44.
[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):41-44.]
|
[15] |
乔彦松, 赵志中, 李增悦, 等. 成都平原红土堆积的风成成因证据[J]. 第四纪研究, 2007, 27(2):286-294.
[QIAO Yansong, ZHAO Zhizhong, LI Zengyue, et al. Aeolian origin of the red earth formation in the Chengdu plain[J]. Quaternary Sciences, 2007, 27(2):286-294.]
|
[16] |
李敬卫, 乔彦松, 王燕, 等. 江西九江红土堆积的粒度特征及其成因研究[J]. 地质力学学报, 2009, 15(1):95-104.
[LI Jingwei, QIAO Yansong, WANG Yan, et al. Aeolian origin of the red earth formation in Jiujiang city of Jiangxi Province, China:evidence from grain-size analysis[J]. Journal of Geomechanics, 2009, 15(1):95-104.]
|
[17] |
刘海丽, 韩志勇, 李徐生, 等. 不同前处理方法对南方红土粒度测量的影响——以安徽宣城第四纪红土剖面为例[J]. 海洋地质与第四纪地质, 2012, 32(2):161-166.
[LIU Haili, HAN Zhiyong, LI Xusheng, et al. Influence of pretreatments on grain-size distribution of the red earth in southern China——A case study on the quaternary red earth profile in Xuancheng, Anhui province[J]. Marine Geology and Quaternary Geology, 2012,32(2):161-166.]
|
[18] |
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 Hexi. Do multiple cycles of aeolian deposit-pedogenesis exist in reticulate red clay sections in southern China[J]. Chinese Science Bulletin, 2003, 48(9):969-975.]
|
[19] |
朱丽东, 叶玮, 周尚哲,等. 金衢盆地第四纪红土沉积粒度组成特征[J]. 海洋地质与第四纪地质, 2006, 26(4):111-116
[ZHU Lidong, YE Wei, ZHOU Shangzhe, et al. Grai-size features of Quaternary red earth in Jinhua-Quzhou Basin[J]. Marine Geology and Quaternary Geology, 200626(4):111-116.]
|
[20] |
杨立辉, 叶玮. 长江中下游第四纪红土中结核的地球化学特征及环境意义[J]. 安徽师范大学学报:自然科学版, 2010, 33(10):567-570.
[YANG Lihui, YE Wei. The geochemistry characters of ferromanganese nodules in the middle and lower reaches of yangtze river[J]. Journal of Anhui Normal University (Natural Science), 2010, 33(10):567-570.]
|
[21] |
刘东生. 黄土与环境[M]. 北京:科学出版社, 1985:191-400.[LIU Tongsheng. Loess and Environment[M]. Beijing:Science Press, 1985:191
-400.]
|
[22] |
何艳花, 苏怀, 董铭,等. 前处理方法对激光粒度仪测试碳酸盐岩红土粒度结果的影响[J]. 土壤通报, 2015, 46(1):148-152.
[HE Yanhua, SU Huai, DONG Ming, et al. The influence of different pretreatment methods on the result of laser particle size analyses for carbonate red soil in Yunnan Plateau[J]. Chinese Journal of Soil Science, 2015, 46(1):148-152.]
|
[23] |
Liu C, Deng C. The effect of weathering on the grain-size distribution of red soils in south-eastern China and its climatic implications[J]. Journal of Asian Earth Sciences, 2014, 94:94-104.
|
[24] |
韩文. 长江中下游红土剖面中黏土矿物的风化淋滤与过渡相结构研究[D]. 中国地质大学, 2014.[HAN Wen. Weathering sequence of clay mineral and structure of intergrade minerals in red earth sediments in the mid-lower reaches of Yangtz River[D]. China University of Geosciences, 2014.]
|
[25] |
唐洪明, 孟英峰, 黎颖英, 等. 高岭石在酸中的化学行为实验研究[J]. 天然气工业, 2006, 26(10):111-113.
[TANG Hongming, MENG Yingfeng, LI Yingying, et al. Experimental research on chemical behavior of kaolin in acid[J]. Natural Gas Industry, 26(10):111-113.]
|
[26] |
王滢, 唐洪明, 杨海博, 等. 富含伊利石的低渗透率砂岩酸化微观实验——以川中某气田须家河组为例[J]. 油气地质与采收率, 2010, 17(1):105-107.
[WANG Ying, TANG Hongming, YANG Haibo, et al. A microcosmic experimental study on acidulation of low permeability sandstone filled with goeschwitzites-a case of Xujiahe Formation, certain gasfield, Central Sichuan[J]. Petroleum Geology and Recovery Efficiency, 2010, 17(1):105-107.]
|