应用指纹识别方法确定泥沙来源研究进展
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摘要
本文介绍了指纹识别方法在泥沙来源研究中的新进展。国际上新近的研究主要针对计算模型的改进和结果的不确定性分析,提出了多种泥沙来源相对贡献率的计算方法,提高了结果的准确性。本文重点介绍了5种指纹识别方法新的计算模型:改进的Collins混合模型、Modified Hughes模型、Landwehr模型、Distribution模型和多元判别分析方法;讨论了不同泥沙来源分区、采样方法和指纹识别因子等对结果不确定性的影响。研究表明通过统计分析方法提高样本数量或使用多指纹识别因子组合可以提高结果的精度。最后,结合实例对多种计算方法进行了分析和比较
This paper reviews the new development of fingerprinting method in sediment research. Recentstudies have focused on the improvement of the models and the uncertainty analysis of the results. In partic-ular,many methods have been proposed to calculate the relative contributions of sediment sources and toimprove the accuracy of the results. At present,there are four new models of fingerprinting method:Modi-fied Hughes,Landwehr,Distribution and Multi-Discriminant Function. The new methods of reducing the un-certainty of results are to improve the accuracy of the results by increasing the number of samples throughstatistical analysis or by using a combination of multiple fingerprinting properties. This paper discusses thefactors that affect the uncertainty of the results:sediment source areas,sampling methods,and fingerprint-ing properties. At last,an application example is given to compare the new models.
This paper reviews the new development of fingerprinting method in sediment research. Recentstudies have focused on the improvement of the models and the uncertainty analysis of the results. In partic-ular,many methods have been proposed to calculate the relative contributions of sediment sources and toimprove the accuracy of the results. At present,there are four new models of fingerprinting method:Modi-fied Hughes,Landwehr,Distribution and Multi-Discriminant Function. The new methods of reducing the un-certainty of results are to improve the accuracy of the results by increasing the number of samples throughstatistical analysis or by using a combination of multiple fingerprinting properties. This paper discusses thefactors that affect the uncertainty of the results:sediment source areas,sampling methods,and fingerprint-ing properties. At last,an application example is given to compare the new models.
引文
[1] COLLINS A L,WALLING D E. Documenting catchment suspended sediment sources:problems,approaches and prospects[J]. Progress in Physical Geography,2004,28:159-196.
[2] WALLING D E. Tracing suspended sediment sources in catchments and river systems[J]. Science of the Total Environment,2005,344:159-184.
[3] OGURI K,HARADA N,TADAI O. Excess210Pb and137Cs concentrations,mass accumulation rates,and sedimentary processes on the Bering Sea continental shelf[J]. Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/64:193-204.
[4] DAVIS C M,FOX J F. Sediment fingerprinting:review of the method and future improvements for allocating nonpoint source pollution[J]. Journal of Environmental Engineering,2009,135(7):490-504.
[5] KOITER A J,OWENS P N,PETTICREW E L,et al. The behavioural characteristics of sediment properties and their implications for sediment fingerprinting as an approach for identifying sediment sources in river basins[J].Earth-Science Reviews,2013,125:24-42.
[6] COLLINS A L,WALLING D E. Selecting fingerprint properties for discriminating potential suspended sediment sources in river basins[J]. Journal of Hydrology,2002,261:218-244.
[7] LONG Y,ZHANG X,WEN A,et al.137Cs fingerprinting technique for erosion and sedimentation studies[J].Journal of Mountain Science,2012,9:34-40.
[8] COLLINS A L,WALLING D E,LEEKS G J L. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique[J]. Catena,1997,29:1-27.
[9] HE Q,WALLING D E. Interpreting particle size effects in the adsorption of137Cs and unsupported210Pb by mineral soils and sediments[J]. Journal of Environmental Radioactivity,1996,30:117-137.
[10]唐强,贺秀斌,鲍玉海,等.泥沙来源“指纹”示踪技术研究综述[J].中国水土保持科学,2013,11(3):109-117.
[11] HADDADCHI A,OLLEY J,LACEBY P. Accuracy of mixing models in predicting sediment source contributions[J]. Science of the Total Environment,2014,497:139-152.
[12] ZHANG X J,ZHANG G H,LIU B L,et al. Using cesium-137 to quantify sediment source contribution and uncertainty in a small watershed[J]. Catena,2016,140:116-124.
[13] MIZUGAKIS,ONDA Y,FUKUYAMA T,et al. Estimation of suspended sediment sources using Cs-137 and Pb-210 in unmanaged Japanese cypress plantation watersheds in southern Japan[J]. Hydrological Processes,2008,22:4519-4531.
[14] GELLIS A C,NOE G B. Sediment source analysis in the Linganore Creek watershed,Maryland,USA,using the sediment fingerprinting approach:2008 to 2010[J]. Journal of Soils and Sediments,2013,13:1735-1753.
[15] HUGHES A O,OLLEY J M,CROKE J C,et al. Sediment source changes over the last 250 years in a dry-tropical catchment,central Queensland,Australia[J]. Geomorphology,2009,104(3):262-275.
[16] COLLINS A L,WALLING D E,WEBB L,et al. Apportioning catchment scale sediment sources using a modified composite fingerprinting technique incorporating property weightings and prior information[J]. Geoderma,2010,155(3/4):249-261.
[17] LACEBY J P,OLLEY J. An examination of geochemical modelling approaches to tracing sediment sources incorporating distribution mixing and elemental correlations[J]. Hydrological Processes,2015,29(6):1669-1685.
[18] LIU B,STORM D E,ZHANG X J,et al. A new method for fingerprinting sediment source contributions using distances from discriminant function analysis[J]. Catena,2016,147:32-39.
[19]林承坤,张德懋,魏特,等.河流推移质泥砂来源和数量计算的方法—岩矿分析计算法[M]//中国地理学会一九七七年地貌学术讨论会.北京:科学出版社,1981.
[20]张信宝,奎因T A,文安邦,等.黄土峁坡农地侵蚀与坡长的关系[J].中国水土保持,1998(1):17-18.
[21]林金石,黄炎和,陈起军,等.组合指纹法研究花岗岩崩岗侵蚀泥沙来源[J].亚热带水土保持,2011,23(4):5-8.
[22]石辉,田均良.利用REE示踪法研究小流域泥沙来源[J].中国科学,1996(5):474-480.
[23]杨明义,徐龙江.黄土高原小流域泥沙来源的复合指纹识别法分析[J].水土保持学报,2010,24(2):30-34.
[24]肖海,刘刚,许文年,等.利用稀土元素示踪三峡库区小流域模型泥沙来源[J].水土保持学报,2014,28(1):47-52.
[25]郑良勇,李占斌,李鹏,等.坡面侵蚀泥沙来源立体分布研究[J].水土保持学报,2012,26(3):58-61.
[26]常维娜,周慧平,高燕.复合指纹识别泥沙来源:潜在泥沙源地的选择[J].生态与农村环境学报,2014,30(6):717-723.
[27] MOTHA J A,WALLBRINK P J,HAIRSINE P B,et al. Unsealed roads as suspended sediment sources in an agricultural catchment in south-eastern Australia[J]. Journal of Hydrology,2004,286(1/4):1-18.
[28] COLLINS A L,WALLING D E,WEBB L,et al. Apportioning catchment scale sediment sources using a modified composite fingerprinting technique incorporating property weightings and prior information[J]. Geoderma,2010,155(3/4):249-261.
[29] OLLEY J,CAITCHEON G. Major element chemistry of sediments from the Darling-Barwon River and its tributaries:implications for sediment and phosphorus sources[J]. Hydrological Processes,2000,14(7):1159-1175.
[30] ZHANG X C,LIU B L. Using multiple composite fingerprints to quantify fine sediment source contributions:A new direction[J]. Geoderma,2016,268:108-118.
[31] BELMONT P,WILLENBRING J K,SCHOTTLER S P,et al. Toward generalizable sediment fingerprinting with tracers that are conservative and nonconservative over sediment routing timescales[J]. Journal of Soils&Sediments,2014,14(8):1479-1492.
[32] NOSRATI K,GOVERS G,SEMMENS B X,et al. A mixing model to incorporate uncertainty in sediment fingerprinting[J]. Geoderma,2014,217/218(3):173-180.
[33] LEES J A. Mineral magnetic properties of mixtures of environmental and synthetic materials:linear additivity and interaction effects[J]. Geophysical Journal of the Royal Astronomical Society,2010,131(2):335-346.
[34] CARTER J,OWENS P N,WALLING D E,et al. Fingerprinting suspended sediment sources in a large urban river system[J]. Science of the Total Environment,2003,314/316:513-534.
[35] PHILLIPS J M,RUSSELL M A,WALLING D E. Time-integrated sampling of fluvial suspended sediment:a simple methodology for small catchments[J]. Hydrological Processes,2015,14(14):2589-2602.
[36] WILKINSON S N,WALLBRINK P J,HANCOCK G J,et al. Fallout radionuclide tracers identify a switch in sediment sources and transport-limited sediment yield following wildfire in a eucalypt forest[J]. Geomorphology,2009,110(3/4):140-151.
[37] BROSINSKY A,FOERSTER S,SEGL K,et al. Spectral fingerprinting:sediment source discrimination and contribution modelling of artificial mixtures based on VNIR-SWIR spectral properties[J]. Journal of Soils&Sediments,2014,14(12):1949-1964.
[38] MARTNEZCARRERAS N,GALLART F,IFFIY J F,et al. Uncertainty Assessment in Suspended Sediment Fingerprinting Based on Tracer Mixing Models:a Case Study from Luxembourg[C]//Conference Sediment Dynamics in Changing Environments. 2008.
[39] SCHIETTECATTE W,GABRIELS D,CORNELIS W M,et al. Enrichment of organic carbon in sediment transport by interrill and rill erosion process[J]. Soil Science Society of America Journal,2008,72(1):50-55.
[40] WILSON C G,KUHNLE R A,BOSCH D D,et al. Quantifying relative contributions from sediment sources in Conservation Effects Assessment Project watersheds[J]. Journal of Soil&Water Conservation,2008,63(6):523-532.
[41] DANIELS R B,GILLIAM J W. Sediment and chemical load reduction by grass and riparian filters[J]. Soil Science Society of America Journal,1996,60(1):246-251.
[42] LIU B,ZHANG X J,STORM D E,et al. Evaluating the WEPP rangeland hillslope model using cesium-137 estimated spatial erosiondata[J].Vadose Zone Journal,2017,16(11).
[2] WALLING D E. Tracing suspended sediment sources in catchments and river systems[J]. Science of the Total Environment,2005,344:159-184.
[3] OGURI K,HARADA N,TADAI O. Excess210Pb and137Cs concentrations,mass accumulation rates,and sedimentary processes on the Bering Sea continental shelf[J]. Deep Sea Research Part II:Topical Studies in Oceanography,2012,61/64:193-204.
[4] DAVIS C M,FOX J F. Sediment fingerprinting:review of the method and future improvements for allocating nonpoint source pollution[J]. Journal of Environmental Engineering,2009,135(7):490-504.
[5] KOITER A J,OWENS P N,PETTICREW E L,et al. The behavioural characteristics of sediment properties and their implications for sediment fingerprinting as an approach for identifying sediment sources in river basins[J].Earth-Science Reviews,2013,125:24-42.
[6] COLLINS A L,WALLING D E. Selecting fingerprint properties for discriminating potential suspended sediment sources in river basins[J]. Journal of Hydrology,2002,261:218-244.
[7] LONG Y,ZHANG X,WEN A,et al.137Cs fingerprinting technique for erosion and sedimentation studies[J].Journal of Mountain Science,2012,9:34-40.
[8] COLLINS A L,WALLING D E,LEEKS G J L. Source type ascription for fluvial suspended sediment based on a quantitative composite fingerprinting technique[J]. Catena,1997,29:1-27.
[9] HE Q,WALLING D E. Interpreting particle size effects in the adsorption of137Cs and unsupported210Pb by mineral soils and sediments[J]. Journal of Environmental Radioactivity,1996,30:117-137.
[10]唐强,贺秀斌,鲍玉海,等.泥沙来源“指纹”示踪技术研究综述[J].中国水土保持科学,2013,11(3):109-117.
[11] HADDADCHI A,OLLEY J,LACEBY P. Accuracy of mixing models in predicting sediment source contributions[J]. Science of the Total Environment,2014,497:139-152.
[12] ZHANG X J,ZHANG G H,LIU B L,et al. Using cesium-137 to quantify sediment source contribution and uncertainty in a small watershed[J]. Catena,2016,140:116-124.
[13] MIZUGAKIS,ONDA Y,FUKUYAMA T,et al. Estimation of suspended sediment sources using Cs-137 and Pb-210 in unmanaged Japanese cypress plantation watersheds in southern Japan[J]. Hydrological Processes,2008,22:4519-4531.
[14] GELLIS A C,NOE G B. Sediment source analysis in the Linganore Creek watershed,Maryland,USA,using the sediment fingerprinting approach:2008 to 2010[J]. Journal of Soils and Sediments,2013,13:1735-1753.
[15] HUGHES A O,OLLEY J M,CROKE J C,et al. Sediment source changes over the last 250 years in a dry-tropical catchment,central Queensland,Australia[J]. Geomorphology,2009,104(3):262-275.
[16] COLLINS A L,WALLING D E,WEBB L,et al. Apportioning catchment scale sediment sources using a modified composite fingerprinting technique incorporating property weightings and prior information[J]. Geoderma,2010,155(3/4):249-261.
[17] LACEBY J P,OLLEY J. An examination of geochemical modelling approaches to tracing sediment sources incorporating distribution mixing and elemental correlations[J]. Hydrological Processes,2015,29(6):1669-1685.
[18] LIU B,STORM D E,ZHANG X J,et al. A new method for fingerprinting sediment source contributions using distances from discriminant function analysis[J]. Catena,2016,147:32-39.
[19]林承坤,张德懋,魏特,等.河流推移质泥砂来源和数量计算的方法—岩矿分析计算法[M]//中国地理学会一九七七年地貌学术讨论会.北京:科学出版社,1981.
[20]张信宝,奎因T A,文安邦,等.黄土峁坡农地侵蚀与坡长的关系[J].中国水土保持,1998(1):17-18.
[21]林金石,黄炎和,陈起军,等.组合指纹法研究花岗岩崩岗侵蚀泥沙来源[J].亚热带水土保持,2011,23(4):5-8.
[22]石辉,田均良.利用REE示踪法研究小流域泥沙来源[J].中国科学,1996(5):474-480.
[23]杨明义,徐龙江.黄土高原小流域泥沙来源的复合指纹识别法分析[J].水土保持学报,2010,24(2):30-34.
[24]肖海,刘刚,许文年,等.利用稀土元素示踪三峡库区小流域模型泥沙来源[J].水土保持学报,2014,28(1):47-52.
[25]郑良勇,李占斌,李鹏,等.坡面侵蚀泥沙来源立体分布研究[J].水土保持学报,2012,26(3):58-61.
[26]常维娜,周慧平,高燕.复合指纹识别泥沙来源:潜在泥沙源地的选择[J].生态与农村环境学报,2014,30(6):717-723.
[27] MOTHA J A,WALLBRINK P J,HAIRSINE P B,et al. Unsealed roads as suspended sediment sources in an agricultural catchment in south-eastern Australia[J]. Journal of Hydrology,2004,286(1/4):1-18.
[28] COLLINS A L,WALLING D E,WEBB L,et al. Apportioning catchment scale sediment sources using a modified composite fingerprinting technique incorporating property weightings and prior information[J]. Geoderma,2010,155(3/4):249-261.
[29] OLLEY J,CAITCHEON G. Major element chemistry of sediments from the Darling-Barwon River and its tributaries:implications for sediment and phosphorus sources[J]. Hydrological Processes,2000,14(7):1159-1175.
[30] ZHANG X C,LIU B L. Using multiple composite fingerprints to quantify fine sediment source contributions:A new direction[J]. Geoderma,2016,268:108-118.
[31] BELMONT P,WILLENBRING J K,SCHOTTLER S P,et al. Toward generalizable sediment fingerprinting with tracers that are conservative and nonconservative over sediment routing timescales[J]. Journal of Soils&Sediments,2014,14(8):1479-1492.
[32] NOSRATI K,GOVERS G,SEMMENS B X,et al. A mixing model to incorporate uncertainty in sediment fingerprinting[J]. Geoderma,2014,217/218(3):173-180.
[33] LEES J A. Mineral magnetic properties of mixtures of environmental and synthetic materials:linear additivity and interaction effects[J]. Geophysical Journal of the Royal Astronomical Society,2010,131(2):335-346.
[34] CARTER J,OWENS P N,WALLING D E,et al. Fingerprinting suspended sediment sources in a large urban river system[J]. Science of the Total Environment,2003,314/316:513-534.
[35] PHILLIPS J M,RUSSELL M A,WALLING D E. Time-integrated sampling of fluvial suspended sediment:a simple methodology for small catchments[J]. Hydrological Processes,2015,14(14):2589-2602.
[36] WILKINSON S N,WALLBRINK P J,HANCOCK G J,et al. Fallout radionuclide tracers identify a switch in sediment sources and transport-limited sediment yield following wildfire in a eucalypt forest[J]. Geomorphology,2009,110(3/4):140-151.
[37] BROSINSKY A,FOERSTER S,SEGL K,et al. Spectral fingerprinting:sediment source discrimination and contribution modelling of artificial mixtures based on VNIR-SWIR spectral properties[J]. Journal of Soils&Sediments,2014,14(12):1949-1964.
[38] MARTNEZCARRERAS N,GALLART F,IFFIY J F,et al. Uncertainty Assessment in Suspended Sediment Fingerprinting Based on Tracer Mixing Models:a Case Study from Luxembourg[C]//Conference Sediment Dynamics in Changing Environments. 2008.
[39] SCHIETTECATTE W,GABRIELS D,CORNELIS W M,et al. Enrichment of organic carbon in sediment transport by interrill and rill erosion process[J]. Soil Science Society of America Journal,2008,72(1):50-55.
[40] WILSON C G,KUHNLE R A,BOSCH D D,et al. Quantifying relative contributions from sediment sources in Conservation Effects Assessment Project watersheds[J]. Journal of Soil&Water Conservation,2008,63(6):523-532.
[41] DANIELS R B,GILLIAM J W. Sediment and chemical load reduction by grass and riparian filters[J]. Soil Science Society of America Journal,1996,60(1):246-251.
[42] LIU B,ZHANG X J,STORM D E,et al. Evaluating the WEPP rangeland hillslope model using cesium-137 estimated spatial erosiondata[J].Vadose Zone Journal,2017,16(11).