[1]霍文,何清,杨兴华,等.中国北方主要沙漠沙尘粒度特征比较研究[J].水土保持研究,2011,18(06):6-11.
　HUO Wen,HE Qing,YANG Xing-hua,et al.The Research on Grain Size Characteristic of Desert in North of China[J].Research of Soil and Water Conservation,2011,18(06):6-11.
点击复制

中国北方主要沙漠沙尘粒度特征比较研究

《水土保持研究》[ISSN:1005-3409/CN:61-1272/P] 卷: 18 期数: 2011年06期 页码: 6-11 栏目: 出版日期: 2011-12-20
Title:
The Research on Grain Size Characteristic of Desert in North of China
作者:
霍文1, 何清1, 杨兴华1, 刘新春1, 丁国锋2, 程玉景3
1. 中国气象局, 乌鲁木齐沙漠气象研究所, 乌鲁木齐 830002;
2. 和静县巴音布鲁克气象站, 新疆, 巴音布鲁克 841314;
3. 库尔勒市气象局, 新疆, 库尔勒 841000
Author(s):
HUO Wen1, HE Qing1, YANG Xing-hua1, LIU Xing-chun1, DING Guo-feng2, CHENG Yu-jing3
1. Institute of Desert and Meteorology, CMA, Urumqi 830002, China;
2. Hejing County Baygnbulak Weather Station, Baygnbulak, Xinjiang 841314, China;
3. Korla Meteorological Bureau, Korla, Xinjiang 841000, China
关键词:
沙漠; 平均粒径; 标准偏差; 偏度; 峰度
Keywords:
desert; mean grain size; standard deviation; skewness; kurtosis
分类号:
P425.5+5
摘要:
粒度分析在区分沉积环境、判定物质输运方式、判别水动力条件和分析粒径趋势等方面具有重要作用。对塔克拉玛干沙漠、库姆塔格沙漠、巴丹吉林沙漠、腾格里沙漠、毛乌素沙地沙尘粒度参数进行了分析比较研究。结果表明：风沙天气过程中，塔中沙漠地区平均粒径Ф值2.95~3.59，标准偏差0.03~0.98；肖塘沙漠过渡带平均粒径Ф值2.93~4.56，标准偏差0.01~0.1；库姆塔格平均粒径Ф值1.55~2.92，标准偏差Ф值0.41~1.11，偏度0.11~0.31，峰度0.77~1.23。巴丹吉林沙漠平均粒径Ф值分别为1.6~1.8，毛乌素沙地为1.7~2.0，腾格里沙漠为1.7~2.3，库布其沙漠为2.1~2.4。库布其沙漠标准偏差Ф值最小0.46~0.51，巴丹吉林沙漠次之为0.55~0.68，腾格里沙漠居中为0.41~0.65，毛乌素最大为0.81~0.91。腾格里沙漠大部分样品为正偏，巴丹吉林与毛乌素为负偏。平均粒径肖塘最小，其次塔中，余下依次为库姆塔格沙漠、库布其、腾格里、毛乌素、巴丹吉林沙漠。肖塘标准偏差Ф值最高，分选最差，其它依次为毛乌素沙漠、塔克拉玛干沙漠、库姆塔格沙漠、腾格里沙漠、巴丹吉林沙漠，库布其分选最好。在频率曲线上反映肖塘、库姆塔格、库布其沙漠细颗粒偏多，塔克拉玛干沙漠、毛乌素、腾格里、巴丹吉林沙漠粗颗粒偏多。
Abstract:
Analysis on grain size of the sediment is very important to differentiate sedimentary environments, determinate the ways of sediment transport, estimate hydrodynamic conditions and analyze grain size trends. Grain size parameters of sand dust in Taklimakan Desert, Kumtag Desert, Badain Jaran Desert, Tengger Desert and Mu Us Sandland were analyzed and compared. The results showed that during sandy and dust weather, the mean grain size values and standard deviation of Tazhong were 2.95～3.95 and 0.03～0.98, respectively, however, those of Xiaotang transition zone were 2.93～4.56 and 0.01～0.1, respectively. The kurtosis value of Xiaotang desert transition zone was higher, and that of Tazhong desert district was lower. The mean grain size values, standard deviation, skewness and kurtosis were 1.55~2.92, 0.41~1.11, 0.11~0.31 and 0.77~1.23, respectively. Mean values of grain size in Badain Jaran Desert, Mu Us Sandland, Tengger Desert and Kubuqi Desert were 1.6~1.8, 1.7~2.0, 1.7~2.3 and 2.1~2.4, respectively. The standard deviation of Kubuqi Desert was the lowest, 0.46~0.51, while the value of Badain Jaran Desert was 0.55～0.68,0.41～0.65 for Tengger Desert, 0.81～0.91 for Mu Us Sandland. Most samples of Tengger Desert positively deviated, while the samples of Badain Jaran Desert and Mu Us Sandland negatively deviated. The orders in lower size to mean grain size were Xiaotang, Tazhong, Kumtag Desert, Kubuqi Desert, Tengger Desert, Mu Us Sandland and Badain Jaran Desert. The orders in higher value to standard deviation were Xiaotang, with the worst sorting features, Mu Us Sandland, Taklimakan Desert, Kumtag Desert, Tengger Desert, Badain Jaran Desert, Kubuqi Desert, with the best sorting features. The distribution frequency shapes reflected that there was more fine silt in Xiaotang, Kumtag Desert and Kubuqi Desert and here was more coarse silt in Taklimakan Desert, Mu Us Sandland, Tengger Desert and Badain Jaran Desert.

参考文献/References:

[1] 刘东生.黄土与环境[M].北京:科学出版社, 1985.
[2] 鹿化煜, 安芷生.黄土高原黄土粒度组成的古气候意义[M].中国科学:D辑, 1998, 28(3):278-283.
[3] 鹿化煜, 安芷生.洛川黄土粒度组成的古气候意义[J].科学通报, 1997, 42(1):66-69.
[4] 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.
[5] Sun Donghuai, An Zhisheng, Su Ruixia, et a1.Eolian sedimentary records for the evolution of monsoon and westerly circulations of northern China in the last 2.6 Ma[J].Science in China:Series D, 2003, 46(10):1049-1059.
[6] Poaer S C, An Zhisheng. Correlation between climate events in the Noah Atlantic and China during the last glaciation[J].Nature, 1995, 375:305-308.
[7] Ding Z, Yu Z, Rutter N W, et a1. Towards an orbital time scale for Chinese loess deposits[J]. Quaternary Sciences Review, 1994, 13:39-70.
[8] Lu Huayu, Li Li, Huang Xiangping, et a1.East Asia winter monsoon oscillation and its correlation with the Noah Atlantic Heinrieh events during the last glaciation[J].Progress in Natural Science, 1996, 6(6):711-717.
[9] 雷国良, 张虎才, 张文翔, 等.Mastersizer 2000型激光粒度仪分析数据可靠性检验及意义:以洛川剖面S4层古土壤为例[J].沉积学报, 2006, 23(4):531-538.
[10] 钱亦兵, 吴兆宁, 陈冬梅, 等.准噶尔中南部沙尘暴源区地表沉积物粒度特征[J].中国沙漠, 2005, 25(6):831-837.
[11] 哈斯.腾格里沙漠东南缘格状沙丘粒度特征与成因探讨[J].地理研究, 1998, 17(2):178-184.
[12] 哈斯, 王贵勇.腾格里沙漠东南缘横向沙丘粒度变化及其与坡面形态的关系[J].中国沙漠, 1996, 16(2):216-221.
[13] 李振山, 陈广庭, 冯起, 等.塔克拉玛干沙漠腹地纵向沙垅表面沙物质粒度特征[J].干旱区资源与环境, 1998, 12(1):21-28.
[14] 陈渭南.塔克拉玛干沙漠84°E沿线沙物质的粒度特征[J].地理学报, 1993, 48(1):33-46.
[15] 钱亦兵, 周华荣, 张立运, 等.塔里木河中下游湿地及其周边土壤粒度的空间分布[J].干旱区地理, 2005, 28(5):609-613.
[16] 吉启慧.粒度分析在塔克拉玛干沙漠研究中的应用[J].中国沙漠, 1996, 16(2):173-179.
[17] 李志忠, 关有志.塔克拉玛干沙漠腹地纵向沙垄的粒度分布特征[J].干旱区研究, 1996, 13(2):37-43.
[18] 钱亦兵, 张希明, 李晓明.塔克拉玛干沙漠南缘绿洲沙物质粒度特征[J].中国沙漠, 1995, 15(2):131-135.
[19] 姚济敏, 张文煜, 袁九毅, 等.典型干旱区沙尘气溶胶光学厚度及粒度谱分布的初步分析[J].中国沙漠, 2006, 26(1):77-80.
[20] 刘树林, 王涛, 郭坚.浑善达克沙地春季风沙活动特征观测研究[J].中国沙漠, 2006, 26(3):356-361.
[21] 李玉霖, 拓万全, 崔建垣.兰州市沙尘和非沙尘天气降尘的粒度特征比较[J].中国沙漠, 2006, 26(4):644-647.
[22] 杨前进.沙尘暴沉降物的粒度特征及其环境意义[J].中国沙漠, 2004, 24(1):47-50.
[23] Folk R L, Ward W C. Brazos river bar: a study in the significance of grain size parameters[J]. Journal of Sedimentary Petrology, 1957, 27:13-26.
[24] 何清, 杨兴华, 霍文, 等.库姆塔格沙漠粒度分布特征及环境意义[J].中国沙漠, 2009, 29(1):18-22.
[25] 霍文, 何清, 刘新春, 等.塔克拉玛干沙漠及其大气降尘点粒度特征分析[J].水土保持研究, 2009, 16(4):207-211.
[26] 丁仲礼, 孙继敏, 刘东生.联系沙漠黄土演变过程中耦合关系的沉积学指标[J].中国科学:D辑, 1999, 29(1):82-87.
[27] 乌兰图雅.科尔沁沙地近50年的垦殖与土地利用变化[J].地理科学进展, 2000, 19(3):273-278.
[28] 邹受益, 张景龙, 冯政夫, 等.科尔沁沙地沙漠化土地初析[J].中国沙漠, 2001, 21(1):76-78.
[29] 张启德, 王玉秀.科尔沁沙地与大气环境[M].北京:科学出版社, 1994.
[30] 岳乐平, 杨利荣, 李智佩, 等.西北地区干枯湖床沉积粒度组成与东亚沙尘天气[J].沉积学报, 2004, 22(2):325-331.

相似文献/References:

[1]刘小燕,朝伦巴根,刘廷玺,等.非饱和带岩性平均粒径的空间变异性研究[J].水土保持研究,2009,16(04):94.
　LIU Xiao-yan,CHAOLUN Ba-gen,LIU Ting-xi,et al.A Study on Spatial Variability of Average Grain Diameter of Rock Formation in Unsaturated Zone[J].Research of Soil and Water Conservation,2009,16(06):94.
[2]霍文,何清,刘新春,等.塔克拉玛干沙漠及其大气降尘点粒度特征分析[J].水土保持研究,2009,16(04):207.
　HUO Wen,HE Qing,LIU Xin-chun,et al.Characteristic of Grain Sizes Atmospheric Dust and Sand in Taklimakan Desert[J].Research of Soil and Water Conservation,2009,16(06):207.

备注/Memo

收稿日期:2011-3-21;改回日期:2011-5-23。
基金项目:公益性行业(气象)科研专项(GYHY201006012);国家“十一五”科技支撑计划项目(2008BAC40B05-01);国家自然基金项目(40975097);中央级公益性科研院所基本科研业务费专项资金项(IDM201001);中国沙漠气象科学研究基金(Sqj2009002)
作者简介:霍文(1981- )，男，陕西人，硕士，助理研究员，从事沙漠气象工作。E-mail：huowenpet@idm.cn

更新日期/Last Update: 1900-01-01