Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China

DONG Yu xiang

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2002 > 20(4): 656-662

DONG Yu xiang. Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China[J]. Acta Sedimentologica Sinica, 2002, 20(4): 656-662.

Citation:

DONG Yu xiang. Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China[J]. Acta Sedimentologica Sinica, 2002, 20(4): 656-662.

Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China

DONG Yu xiang

Department of Geography,Zhongshan University, Guangzhou 510275

Received Date: 2001-11-12
Rev Recd Date: 2002-06-25

Abstract

The characteristics of grain size parameters of modern coastal aeolian sands are the basic problems of coastal aeolian sand research. This paper, taking the temperate coastal zone in China as an example, makes use of the grain size parameter such as component of grain size, mean size, standard deviation, skewnss and kurtosis to study the characteristics of grain size parameters of modern coastal aeolian sands on the basis of data of 136 grain size samples. The research results can be concluded that the modern coastal aeolian sands in the temperate coastal zone in China are not all composed of fine sands with high sorting degree which were thought as before. Most are positively skewed. The parameters of grain size clearly change in different coastal zones and change with different sand dune type and dune size as well as distance from coastal line. Compared with beach sands, dune sands have the characteristics of contenting silt, thinner, more positive skewness and sharper kurtosis, but the beach sands and the dune sands in the temperate coastal zone in China can not be distinguished by use of the parameter plot of grain size and component analysis method. These characteristics of modern dune sands in the temperate coastal zone in China are connected with the special physical conditions and evolution process of the temperate coastal zone in China, in which the clear monsoon climate and short formation time as well as narrow space for aeolian activities play leading role in the formation of characteristics above.
- coastal zone,
- modern aeolian sands,
- grain size,
- temperate zone in China

References

[1]	Mason C C, Folk R L. Differentiation of beach, dune and Aeolian flat environment by size analysis, Mustang Island, Texas[J]. Journal of Sedimentary Petrology, 1958, 28(2): 211～226
[2]	Friedmen M F. Distinction between dune, beach, and river sands from their textural characteristics[J]. Journal of Sedimentary Petrology, 1961, 31(4): 514～529
[3]	Shepard F P, Young R. Distinguishing between beach and dune sands[J]. Journal of Sedimentary Petrology, 1961, 31(2): 196～214
[4]	Martins L R. Significance of skewness and kurtosis in environmental interpretation[J]. Journal of Sedimentary Petrology, 1965, 35: 768～770
[5]	Moiola R J, Weiser D. Texture parameter: an evolution[J]. Journal of Sedimentary Petrology, 1968, 38(1): 45～53
[6]	Bigarella J J, Becker R D, Duarte G M. Coastal dune structures from Parana Brazil[J]. Marine Geology, 1969, 7(1): 5～55
[7]	Bigarella J J. Eolian environments: their characteristics, recognitions and importance[A]. In: Rigby J K, Hamblin W K, eds. Recognition of ancient sedimentary environment[C]. Soc. Econ. Paleontologists and Mineralogists Spec. Pub., 1972, 16: 12～62
[8]	Friedman G M. Textural parameters of sands-useful or useless?[J] Geol. Soc. America Abs. With Programs, 1973, 5(7): 626～627
[9]	Moilila R J, Spencer A B, Mckee E D. Linear discriminant analysis-a technique for analyzing sand bodies[J]. Geol. Soc. America Abs. With Programs, 1973, 5(7): 741～742
[10]	Moilila R J, Spencer A B, Weiser D. Differentiation of modern sand bodies by linear discriminant analysis[J]. Gulf Coast Assoc. Geol. Socs. Trans., 1974, 24: 321～326
[11]	Davis Jr R A. Coastal sedimentary environments[M]. New York: Springer-Verlag, 1978, 304～378
[12]	Mckee E D. A study of the global sand seas. U S.[M]. Washington: Government Printing Office, 1979
[13]	Pye K. Negatively shewed aeolian sands from a human tropical coastal dunefield, Northern Australia[J]. Sedimentary Geology, 1982, 31:249～266
[14]	Pye K. Coastal dune. Progress in Physical Geography[C]. 1983, 7(4): 531～557
[15]	Lancaster N. The Namib sand sea: dunes forms, processes and sediments[C]. Balkema A. ed. 1989, 46～80
[16]	Pye K, Tosar H. Aeolian sand and sand dunes[M]. Unwin Hyman, 1990
[17]	Nordstrom K, Psuty N, Caeter B. Coastal dune: form and process[M]. John Wiley & Sons, 1990
[18]	Pye K, Lancaster N. Aeolian sediments: ancient and modern[M]. Blackwell, 1993
[19]	Linvingstone I, Warren A. Aeolian geomorphology: an introduction[M]. Longman, 1996
[20]	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(1): 3～26
[21]	周莉.山东半岛浅滩沙、河流沙和沙丘沙粒度频率分布和统计参数的环境意义[J].山东海洋学院学报,1979,(2): 39～49[Zhou Li. Environmental significance of frequency distribution and parameters of grain size of beach sand,river sand and dune sand in Shandong Peninsula[J]. Journal of Shandong Ocean College,1979,(2):39～49]
[22]	高善明,李元芳,安凤桐等.滦河三角洲滨岸沙体的形成和海岸线变迁[J].海洋学报,1980,2(4): 102～114[Gao Shanming, Li Yuan fang, An Fengtong. The formation of sand bars on the Luanhe river delta and the change of the coast line[J].Acta Oceanologica Sinica, 1980,2(4):102～114]
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[26]	李从先,陈刚,王秀强.滦河以北海岸风成砂沉积的初步研究[J].中国沙漠,1987,7(2): 12～21[Li Congxian, Chen Gang, Wang Xiuqiang. Study on coastal sand sedimentation at the north bank of Luanhe river[J]. Journal of Desert Research,1987,7(2):12～21 ]
[27]	王颖,朱大奎.海岸沙丘成因的讨论[J].中国沙漠,1987,7(3): 29～40[Wang Ying, Zhu Dakui. An approach on the formation causes of coastal sand dunes[J]. Journal of Desert Research,1987,7(3):29～40]
[28]	赵希涛,沙庆安,Goldsmith V等. 福建莆田海岸沙丘岩--Ⅰ.沉积构造与古风[J].中国科学(B辑),1988,(11): 196～205[Zhao Xitao, Sha Qngan, Goldsmith V, et al. Coastal dune rqcks in Putian of Fujian Province[J]. Science in China(Series B), 1988,(11):196～205]
[29]	李从先,陈刚,杨红君.福建海岸的风成沉积[J].中国沙漠,1989,9(4): 8～18[Li Congxian, Chen Gang, Yang Hongjun. Eolina deposits in coastal zones of Fujian Province[J]. Journal of Desert Research,1989,9(4):8～18]
[30]	陈方.长乐东部沿岸风沙沉积物的粒度分布特征[J].福建师范大学学报(自然科学版),1991,7(2):84～91[Chen Fang. The distribution characterisitics of grain size of coastal aeolian sediments in eastern beach of Changle[J]. Journal of Fujian Normal University, 1991, 7(2):84～91]
[31]	傅启龙,沙庆安.昌黎海岸风成沙丘组构特征及其与海滩砂的比较[J].地质科学,1993,28(1): 52～59[Fu Qilong, Sha Qingan. A comparative study on textural characteristic of dune and beach sands on the coast of Changli Hebei[J]. Scientia Geologica Sinica, 1993, 28(1):52～59]
[32]	吴正,黄山,胡守真等.华南海岸风沙地貌研究[J].北京:科学出版社,1995. 59～63[Wu Zheng, Huang Shan, Hu Shouzhen, et al. Research on the landforms of the wind-drift sand in south Chian coast[J]. Beijing:Science Press, 1995. 59～63]
[33]	王月霄. 昌黎黄金海岸沙丘沉积特征及形成演变[J].地理学与国土研究,1996,12(3): 60～64[Wang Yuexiao. The characterstics of Changli golden coastal dune deposit and its formation and change[J]. Geography and Territorial Research,1999,12(3):60～64]
[34]	董玉祥.中国温带海岸沙丘分类系统初步探讨[J].中国沙漠,2000,20(2): 159～165[Dong Yuxiang. Classification of coastal dunes in temperate zone in China[J]. Journal of Desert Research, 2000, 20(2): 159～165]
[35]	傅命佐,徐孝诗,徐小薇.黄、渤海海岸风沙地貌类型及其分布规律和发育模式[J].海洋与湖沼,1997,28(1): 56～65[Fu Mingzuo,Xu Xiaoshi,Xu Xiaowei. The aeolian geomorphical types in the coastal areas of the Yellow Sea and Bohai Sea and their distribution patterns and development models[J]. Oceanologica et Limnologica Sinica, 1997, 28(1):56～65]
[36]	胡镜荣.旅游沙丘因子和临界容量[J].地理学与国土研究,1999,15(1):61～64[Hu Jingrong. Tourism sand dune factor and critical capactiy[J]. Geography and Territorial Research, 1999, 15(1): 61～64]
[37]	赵松龄,于红军.晚更新世末期黄、渤海陆架沙漠化环境的形成[J].第四纪研究,1996,(1):42～47[Zhao Songliang, Yu Hongjun. Shelf desertization environment in the Baohai and Yellow seas during the last glacial maximum[J]. Quaternary Sciences, 1996, (1):42～47]
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Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China

Department of Geography,Zhongshan University, Guangzhou 510275

Received Date: 2001-11-12

Rev Recd Date: 2002-06-25

Key words:

Abstract: The characteristics of grain size parameters of modern coastal aeolian sands are the basic problems of coastal aeolian sand research. This paper, taking the temperate coastal zone in China as an example, makes use of the grain size parameter such as component of grain size, mean size, standard deviation, skewnss and kurtosis to study the characteristics of grain size parameters of modern coastal aeolian sands on the basis of data of 136 grain size samples. The research results can be concluded that the modern coastal aeolian sands in the temperate coastal zone in China are not all composed of fine sands with high sorting degree which were thought as before. Most are positively skewed. The parameters of grain size clearly change in different coastal zones and change with different sand dune type and dune size as well as distance from coastal line. Compared with beach sands, dune sands have the characteristics of contenting silt, thinner, more positive skewness and sharper kurtosis, but the beach sands and the dune sands in the temperate coastal zone in China can not be distinguished by use of the parameter plot of grain size and component analysis method. These characteristics of modern dune sands in the temperate coastal zone in China are connected with the special physical conditions and evolution process of the temperate coastal zone in China, in which the clear monsoon climate and short formation time as well as narrow space for aeolian activities play leading role in the formation of characteristics above.

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Reference (45)

[1]	Mason C C, Folk R L. Differentiation of beach, dune and Aeolian flat environment by size analysis, Mustang Island, Texas[J]. Journal of Sedimentary Petrology, 1958, 28(2): 211～226
[2]	Friedmen M F. Distinction between dune, beach, and river sands from their textural characteristics[J]. Journal of Sedimentary Petrology, 1961, 31(4): 514～529
[3]	Shepard F P, Young R. Distinguishing between beach and dune sands[J]. Journal of Sedimentary Petrology, 1961, 31(2): 196～214
[4]	Martins L R. Significance of skewness and kurtosis in environmental interpretation[J]. Journal of Sedimentary Petrology, 1965, 35: 768～770
[5]	Moiola R J, Weiser D. Texture parameter: an evolution[J]. Journal of Sedimentary Petrology, 1968, 38(1): 45～53
[6]	Bigarella J J, Becker R D, Duarte G M. Coastal dune structures from Parana Brazil[J]. Marine Geology, 1969, 7(1): 5～55
[7]	Bigarella J J. Eolian environments: their characteristics, recognitions and importance[A]. In: Rigby J K, Hamblin W K, eds. Recognition of ancient sedimentary environment[C]. Soc. Econ. Paleontologists and Mineralogists Spec. Pub., 1972, 16: 12～62
[8]	Friedman G M. Textural parameters of sands-useful or useless?[J] Geol. Soc. America Abs. With Programs, 1973, 5(7): 626～627
[9]	Moilila R J, Spencer A B, Mckee E D. Linear discriminant analysis-a technique for analyzing sand bodies[J]. Geol. Soc. America Abs. With Programs, 1973, 5(7): 741～742
[10]	Moilila R J, Spencer A B, Weiser D. Differentiation of modern sand bodies by linear discriminant analysis[J]. Gulf Coast Assoc. Geol. Socs. Trans., 1974, 24: 321～326
[11]	Davis Jr R A. Coastal sedimentary environments[M]. New York: Springer-Verlag, 1978, 304～378
[12]	Mckee E D. A study of the global sand seas. U S.[M]. Washington: Government Printing Office, 1979
[13]	Pye K. Negatively shewed aeolian sands from a human tropical coastal dunefield, Northern Australia[J]. Sedimentary Geology, 1982, 31:249～266
[14]	Pye K. Coastal dune. Progress in Physical Geography[C]. 1983, 7(4): 531～557
[15]	Lancaster N. The Namib sand sea: dunes forms, processes and sediments[C]. Balkema A. ed. 1989, 46～80
[16]	Pye K, Tosar H. Aeolian sand and sand dunes[M]. Unwin Hyman, 1990
[17]	Nordstrom K, Psuty N, Caeter B. Coastal dune: form and process[M]. John Wiley & Sons, 1990
[18]	Pye K, Lancaster N. Aeolian sediments: ancient and modern[M]. Blackwell, 1993
[19]	Linvingstone I, Warren A. Aeolian geomorphology: an introduction[M]. Longman, 1996
[20]	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(1): 3～26
[21]	周莉.山东半岛浅滩沙、河流沙和沙丘沙粒度频率分布和统计参数的环境意义[J].山东海洋学院学报,1979,(2): 39～49[Zhou Li. Environmental significance of frequency distribution and parameters of grain size of beach sand,river sand and dune sand in Shandong Peninsula[J]. Journal of Shandong Ocean College,1979,(2):39～49]
[22]	高善明,李元芳,安凤桐等.滦河三角洲滨岸沙体的形成和海岸线变迁[J].海洋学报,1980,2(4): 102～114[Gao Shanming, Li Yuan fang, An Fengtong. The formation of sand bars on the Luanhe river delta and the change of the coast line[J].Acta Oceanologica Sinica, 1980,2(4):102～114]
[23]	蔡爱智,蔡月娥.中国海岸风沙沉积的成因与特征[J].中国沙漠,1983,3(3): 1～10[Cai Aizhi,Cai Yuee. A study of depositional causation and characteristics of coast aeolian sand in coast areas in China[J]. Journal of Desert Research, 1983, 3(3):1～10]
[24]	李善为,刘敏厚,王永吉等.山东半岛海岸的风成沙丘[J].黄渤海海洋,1985,3(3): 47～56[Li Shanwei, Liu Minhou, Wang Yongji, et al. Wind-induces dunes along the coast of Shangdong Peninsula[J]. Journal of Oceanography of Huanghai Bohai Seas,1985,3(3):47～56]
[25]	吕浩雪.冀东海岸沉积物粒度分析及其沉积环境解释[J].南京大学学报(地理学),1986,55～63[Lu Haoxue. An analysis for the grain size of sediments and the explanation of depositional environment in Jidong shore of Hebei plain[J]. Journal of Nanjing University (Geography edition), 1986,55～63]
[26]	李从先,陈刚,王秀强.滦河以北海岸风成砂沉积的初步研究[J].中国沙漠,1987,7(2): 12～21[Li Congxian, Chen Gang, Wang Xiuqiang. Study on coastal sand sedimentation at the north bank of Luanhe river[J]. Journal of Desert Research,1987,7(2):12～21 ]
[27]	王颖,朱大奎.海岸沙丘成因的讨论[J].中国沙漠,1987,7(3): 29～40[Wang Ying, Zhu Dakui. An approach on the formation causes of coastal sand dunes[J]. Journal of Desert Research,1987,7(3):29～40]
[28]	赵希涛,沙庆安,Goldsmith V等. 福建莆田海岸沙丘岩--Ⅰ.沉积构造与古风[J].中国科学(B辑),1988,(11): 196～205[Zhao Xitao, Sha Qngan, Goldsmith V, et al. Coastal dune rqcks in Putian of Fujian Province[J]. Science in China(Series B), 1988,(11):196～205]
[29]	李从先,陈刚,杨红君.福建海岸的风成沉积[J].中国沙漠,1989,9(4): 8～18[Li Congxian, Chen Gang, Yang Hongjun. Eolina deposits in coastal zones of Fujian Province[J]. Journal of Desert Research,1989,9(4):8～18]
[30]	陈方.长乐东部沿岸风沙沉积物的粒度分布特征[J].福建师范大学学报(自然科学版),1991,7(2):84～91[Chen Fang. The distribution characterisitics of grain size of coastal aeolian sediments in eastern beach of Changle[J]. Journal of Fujian Normal University, 1991, 7(2):84～91]
[31]	傅启龙,沙庆安.昌黎海岸风成沙丘组构特征及其与海滩砂的比较[J].地质科学,1993,28(1): 52～59[Fu Qilong, Sha Qingan. A comparative study on textural characteristic of dune and beach sands on the coast of Changli Hebei[J]. Scientia Geologica Sinica, 1993, 28(1):52～59]
[32]	吴正,黄山,胡守真等.华南海岸风沙地貌研究[J].北京:科学出版社,1995. 59～63[Wu Zheng, Huang Shan, Hu Shouzhen, et al. Research on the landforms of the wind-drift sand in south Chian coast[J]. Beijing:Science Press, 1995. 59～63]
[33]	王月霄. 昌黎黄金海岸沙丘沉积特征及形成演变[J].地理学与国土研究,1996,12(3): 60～64[Wang Yuexiao. The characterstics of Changli golden coastal dune deposit and its formation and change[J]. Geography and Territorial Research,1999,12(3):60～64]
[34]	董玉祥.中国温带海岸沙丘分类系统初步探讨[J].中国沙漠,2000,20(2): 159～165[Dong Yuxiang. Classification of coastal dunes in temperate zone in China[J]. Journal of Desert Research, 2000, 20(2): 159～165]
[35]	傅命佐,徐孝诗,徐小薇.黄、渤海海岸风沙地貌类型及其分布规律和发育模式[J].海洋与湖沼,1997,28(1): 56～65[Fu Mingzuo,Xu Xiaoshi,Xu Xiaowei. The aeolian geomorphical types in the coastal areas of the Yellow Sea and Bohai Sea and their distribution patterns and development models[J]. Oceanologica et Limnologica Sinica, 1997, 28(1):56～65]
[36]	胡镜荣.旅游沙丘因子和临界容量[J].地理学与国土研究,1999,15(1):61～64[Hu Jingrong. Tourism sand dune factor and critical capactiy[J]. Geography and Territorial Research, 1999, 15(1): 61～64]
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[38]	赵希涛.中国贝壳堤发育及其对海岸线变迁的反映[J].地理科学,1986,6(4):294～304[Zhao Xitao. Development of Cheniers in China and their reflection on the coastline shift[J]. Scientia Geographica, 1986, 6(4):294～304]
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Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China

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