Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province

WANG Ai jun; WANG Ya ping; YANG Yang

Article Contents

Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(1): 124-129

WANG Ai jun, WANG Ya ping, YANG Yang. Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province[J]. Acta Sedimentologica Sinica, 2004, 22(1): 124-129.

Citation:

WANG Ai jun, WANG Ya ping, YANG Yang. Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province[J]. Acta Sedimentologica Sinica, 2004, 22(1): 124-129.

Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province

Ministry of Education Key Laboratory for Coast and Islands Development,Nanjing University, Nanjing 210093

Received Date: 2003-02-10
Rev Recd Date: 2003-04-06
Publish Date: 2004-03-10

Abstract

Sediment parameters of inter tidal flat are related to the depositional hydrodynamic conditions associated with the local sedimentary environment. During July August, 2000, 154 surface sediment samples were collected on the intertidal flat of Wanggang. The sediment samples are then analyzed using Mastersize2000. Further, the regression analysis shows that the significant relationships are present between the sediment parameters, and as well with ( M z Φ M d Φ). In addition, the grain size diameters decrease landward with the decreasing of the hydrodynamics. Five types of sediments have been identified for the Wanggang intertidal flat:fine sand, silty sand, sandy silt, silt and clayey silt. In brief, there are two main sediment types, i.e. silt and sand with the percentages of 57.8% and 42.2% respectively. These results differ from other intertidal flats associated with different sediment sources, hydrodynamic environments and bio influences. The results of grain size trends show that the sediments mainly transport northwestward near the sub tidal zone; but southward, southwestward and southeastward, which are related to tide regimes, local landscape, large human constructions and the biological activities.
- Sediment types,
- grain size parameters,
- grain size trends analysi\Wanggang inter tidal flat,

References

[1]	Halls J R. Significance of statistical parameters for distinguishing sedimentary environments in New South Wales, Australia. Journal of Sedimentary Petrology, 1967,37:1059～1069
[2]	Wang X Y, Ke X K. Grain size characteristics of the extant tidal flat sediments along the Jiangsu coast, China. Sedimentary Geology, 1997, 112:105～122
[3]	Friedman G M. Address of retiring President of the International Association of Sedimentology:difference in size distributions of populations of particles among sands from various origins. Sedimentology, 1979, 26: 3～22
[4]	Mclaren P, Bowles D. The effects of sediment transport on grain-size distributions. Journal of Sedimentary Petrology, 1985,55:457～470
[5]	Gao S, Collins M B. Net sediment transport patterns inferred from grain-size trends, based upon definition of "transport vectors". Sedimentary Geology, 1992,81(3/4):47～60
[6]	Gao S, Collins M B, Lanckneus J, et al. Grain size trends associated with net sediment transport patterns:an example from the Belgian continental shelf. Marine Geology, 1994, 121:171～185
[7]	汪亚平, 高抒, 贾建军. 胶州湾及邻近海域沉积物分布特征和运移趋势. 地理学报, 2000,55(4):449～458[Wang Y P, Gao S, Jia J J. Sediment distribution and transport patterns in Jiaozhou Bay and adjoining areas. Acta Geographica Sinica, 2000, 55(4):449～458]
[8]	薛允传, 贾建军, 高抒. 山东月湖的沉积物分布特征和搬运趋势. 地理研究,2002,21(6):707～714[Xue Y C, Jia J J, Gao S. Sediment distribution and transport patterns in Lagoon Yuehu at the eastern tip of Shandong Peninsula, China. Geographical Research, 2002,21(6):707～714]
[9]	Ren M E, Zhang R S, Yang J H. Sedimentation on tidal mud flat of Wanggang Area, Jiangsu Province, China. Collected Oceanic Works, 1983, 6(2):84～108
[10]	任美锷主编. 江苏省海岸带和海涂资源综合调查. 北京:海洋出版社,1986,25～37[Ren M E, ed. Comprehensive Investigation of the Coastal Zone and Tidal Flat Resources of Jiangsu Province. Beijing:Ocean Press, 1986, 25～37]
[11]	Shepard F P. Nomenclature based on sand-silt-clay ratios. Journal of Sedimentary Petrology, 1954, 24:151～158
[12]	McManus J. Grain size determination and interpretation. In: Techniques in Sedimentology. Oxford: Blackwell, 1988. 63～85
[13]	贾建军, 高抒, 薛允传. 图解法与矩法沉积物粒度参数的对比. 海洋与湖沼,2002,33(6):577～582[Jia J J, Gao S, Xue Y C. Grain size parameters derived from graphic and moment methods:a comparative study. Oceanologia et Limnologia Sinica, 2002, 23(6):577～582]
[14]	Evans G. Intertidal flat sediments and their environments of deposition in the Wash. Quarterly Journal of Geological Society of London, 1965, 121:209～245
[15]	De Jong J D. Dutch tidal flat. Sedimentary Geology, 1977,18:13～23
[16]	Davis R A. Coastal Sedimentary Environments (2nd). New York: Springer-Verlag Inc, 1985. 208～213
[17]	Alexander C R. Macro-tidal mudflats of the southwestern Korean coast: a model for interpretation of inter-tidal deposits. Journal of Sedimentary Petrology, 1991,61:805～824
[18]	Reineck H-E, Singh I B. Depositional Sedimentary Environments(2nd Ed.). Berlin: Springer, 1980. 430～456
[19]	Ke X K, Evans G, Collins M B. Hydrodynamics and sediment dynamics of the Wash embayment, eastern England. Sedimentology, 1996, 43:157～174
[20]	Malvarez G C, Cooper J A G, Jackson D W T. Relationships between wave-induced currents and sediment grain size on a sandy tidal-flat. Journal of Sedimentary Research, 2001, 71:705～712
[21]	Bartholdy J, Madsen P P. Accumulation of fine-grained material in a Danish tidal area. Marine Geology, 1985, 67: 121～137
[22]	Janssen-Stelder B. The effect of different hydrodynamic conditions on the morphodynamics of a tidal mudflat in the Dutch Wadden Sea. Continental Shelf Research, 2000, 20:1461～1478
[23]	Klein G D. Bay of Fundy intertidal zone sediments. Journal of Sedimentary Petrology, 1963, 33:844～854
[24]	Pestrong R. Tidal-flat sedimentation at Cooley landing, Southwest San Francisco Bay. Sedimentary Geology, 1972,8:251～288
[25]	Stumpf R P. The process of sedimentation on the surface of a salt marsh. Estuarine, Coastal and Shelf Science, 1983, 17:495～508
[26]	Augustinus P G. Actual development of the chenier coast of Suriname (South America). Sedimentary Geology, 1980,26:91～113
[27]	Anthony E J. Coastal progradation in response to variations in sediment supply, wave energy and tidal range: examples from Sierra Leone, West Africa. Geodynamique, 1991,6(1):57～70
[28]	Le Hir P, Roberts W, Cazaillet O, et al. Characterization of intertidal flat hydrodynamics. Continental Shelf Research, 2000, 20:1433～1459
[29]	朱晓东, 施丙文, 朱大奎. 一种适用于微体古生物沉积动力分析的沉积物粒径指数及其应用例证. 沉积学报,1997, 15(3):145～149[Zhu X D, Shi B W, Zhu D K. A new sediment grain size index designed for sedimentological study of microfossils-with demonstrations of foraminifera in Jiangsu Coast, China. Acta Sedimentological Sinica, 1997, 15(3):145～149

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Get Citation

PDF

XML

Article Metrics

Article views(555) PDF downloads(496) Cited by()

Proportional views

Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province

Ministry of Education Key Laboratory for Coast and Islands Development,Nanjing University, Nanjing 210093

Received Date: 2003-02-10

Rev Recd Date: 2003-04-06

Publish Date: 2004-03-10

Key words:

Sediment types /
grain size parameters /
grain size trends analysi\Wanggang inter tidal flat /

Abstract: Sediment parameters of inter tidal flat are related to the depositional hydrodynamic conditions associated with the local sedimentary environment. During July August, 2000, 154 surface sediment samples were collected on the intertidal flat of Wanggang. The sediment samples are then analyzed using Mastersize2000. Further, the regression analysis shows that the significant relationships are present between the sediment parameters, and as well with ( M z Φ M d Φ). In addition, the grain size diameters decrease landward with the decreasing of the hydrodynamics. Five types of sediments have been identified for the Wanggang intertidal flat:fine sand, silty sand, sandy silt, silt and clayey silt. In brief, there are two main sediment types, i.e. silt and sand with the percentages of 57.8% and 42.2% respectively. These results differ from other intertidal flats associated with different sediment sources, hydrodynamic environments and bio influences. The results of grain size trends show that the sediments mainly transport northwestward near the sub tidal zone; but southward, southwestward and southeastward, which are related to tide regimes, local landscape, large human constructions and the biological activities.

HTML

Reference (29)

[1]	Halls J R. Significance of statistical parameters for distinguishing sedimentary environments in New South Wales, Australia. Journal of Sedimentary Petrology, 1967,37:1059～1069
[2]	Wang X Y, Ke X K. Grain size characteristics of the extant tidal flat sediments along the Jiangsu coast, China. Sedimentary Geology, 1997, 112:105～122
[3]	Friedman G M. Address of retiring President of the International Association of Sedimentology:difference in size distributions of populations of particles among sands from various origins. Sedimentology, 1979, 26: 3～22
[4]	Mclaren P, Bowles D. The effects of sediment transport on grain-size distributions. Journal of Sedimentary Petrology, 1985,55:457～470
[5]	Gao S, Collins M B. Net sediment transport patterns inferred from grain-size trends, based upon definition of "transport vectors". Sedimentary Geology, 1992,81(3/4):47～60
[6]	Gao S, Collins M B, Lanckneus J, et al. Grain size trends associated with net sediment transport patterns:an example from the Belgian continental shelf. Marine Geology, 1994, 121:171～185
[7]	汪亚平, 高抒, 贾建军. 胶州湾及邻近海域沉积物分布特征和运移趋势. 地理学报, 2000,55(4):449～458[Wang Y P, Gao S, Jia J J. Sediment distribution and transport patterns in Jiaozhou Bay and adjoining areas. Acta Geographica Sinica, 2000, 55(4):449～458]
[8]	薛允传, 贾建军, 高抒. 山东月湖的沉积物分布特征和搬运趋势. 地理研究,2002,21(6):707～714[Xue Y C, Jia J J, Gao S. Sediment distribution and transport patterns in Lagoon Yuehu at the eastern tip of Shandong Peninsula, China. Geographical Research, 2002,21(6):707～714]
[9]	Ren M E, Zhang R S, Yang J H. Sedimentation on tidal mud flat of Wanggang Area, Jiangsu Province, China. Collected Oceanic Works, 1983, 6(2):84～108
[10]	任美锷主编. 江苏省海岸带和海涂资源综合调查. 北京:海洋出版社,1986,25～37[Ren M E, ed. Comprehensive Investigation of the Coastal Zone and Tidal Flat Resources of Jiangsu Province. Beijing:Ocean Press, 1986, 25～37]
[11]	Shepard F P. Nomenclature based on sand-silt-clay ratios. Journal of Sedimentary Petrology, 1954, 24:151～158
[12]	McManus J. Grain size determination and interpretation. In: Techniques in Sedimentology. Oxford: Blackwell, 1988. 63～85
[13]	贾建军, 高抒, 薛允传. 图解法与矩法沉积物粒度参数的对比. 海洋与湖沼,2002,33(6):577～582[Jia J J, Gao S, Xue Y C. Grain size parameters derived from graphic and moment methods:a comparative study. Oceanologia et Limnologia Sinica, 2002, 23(6):577～582]
[14]	Evans G. Intertidal flat sediments and their environments of deposition in the Wash. Quarterly Journal of Geological Society of London, 1965, 121:209～245
[15]	De Jong J D. Dutch tidal flat. Sedimentary Geology, 1977,18:13～23
[16]	Davis R A. Coastal Sedimentary Environments (2nd). New York: Springer-Verlag Inc, 1985. 208～213
[17]	Alexander C R. Macro-tidal mudflats of the southwestern Korean coast: a model for interpretation of inter-tidal deposits. Journal of Sedimentary Petrology, 1991,61:805～824
[18]	Reineck H-E, Singh I B. Depositional Sedimentary Environments(2nd Ed.). Berlin: Springer, 1980. 430～456
[19]	Ke X K, Evans G, Collins M B. Hydrodynamics and sediment dynamics of the Wash embayment, eastern England. Sedimentology, 1996, 43:157～174
[20]	Malvarez G C, Cooper J A G, Jackson D W T. Relationships between wave-induced currents and sediment grain size on a sandy tidal-flat. Journal of Sedimentary Research, 2001, 71:705～712
[21]	Bartholdy J, Madsen P P. Accumulation of fine-grained material in a Danish tidal area. Marine Geology, 1985, 67: 121～137
[22]	Janssen-Stelder B. The effect of different hydrodynamic conditions on the morphodynamics of a tidal mudflat in the Dutch Wadden Sea. Continental Shelf Research, 2000, 20:1461～1478
[23]	Klein G D. Bay of Fundy intertidal zone sediments. Journal of Sedimentary Petrology, 1963, 33:844～854
[24]	Pestrong R. Tidal-flat sedimentation at Cooley landing, Southwest San Francisco Bay. Sedimentary Geology, 1972,8:251～288
[25]	Stumpf R P. The process of sedimentation on the surface of a salt marsh. Estuarine, Coastal and Shelf Science, 1983, 17:495～508
[26]	Augustinus P G. Actual development of the chenier coast of Suriname (South America). Sedimentary Geology, 1980,26:91～113
[27]	Anthony E J. Coastal progradation in response to variations in sediment supply, wave energy and tidal range: examples from Sierra Leone, West Africa. Geodynamique, 1991,6(1):57～70
[28]	Le Hir P, Roberts W, Cazaillet O, et al. Characterization of intertidal flat hydrodynamics. Continental Shelf Research, 2000, 20:1433～1459
[29]	朱晓东, 施丙文, 朱大奎. 一种适用于微体古生物沉积动力分析的沉积物粒径指数及其应用例证. 沉积学报,1997, 15(3):145～149[Zhu X D, Shi B W, Zhu D K. A new sediment grain size index designed for sedimentological study of microfossils-with demonstrations of foraminifera in Jiangsu Coast, China. Acta Sedimentological Sinica, 1997, 15(3):145～149

Surface Sediment Characteristics and Transport Trends on the Wanggang Intertidal Flat,Jiangsu Province

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

Article Metrics

Proportional views

Related