Author(s)

H.N. Pansambal

Affiliation(s)

Department of Chemistry, Shri Saibaba College Shirdi, 423 109, Savitribai Phule Pune University, Maharashtra, India.

Corresponding Author

H.N. Pansambal

ABSTRACT

Floodplain deposits are deposits formed when rivers flood the plain., is an important carrier for watershed environmental research. in recent years, related to floodplain sedimentation Environmental research involves watershed environmental evolution, ancient flood, environmental archeology and flow area ring territory Sewage dye and flow area ring territory back scene wait collar area. return Forget it 20th century discipline 80 years The main progress in floodplain sedimentation and environmental research over the past generations, focusing on the beach sink product much Sample sex and sink product special levy, river comic beach sink accumulation ring territory refer to mark of meaning righteous, The application of floodplain sedimentation in paleoflood and watershed environmental pollution research is reviewed and analyzed., Consider floodplain sedimentation to be diverse and complex, Floodplain sedimentation has made great achievements in ancient flood research and basin environmental pollution. big quantity research study become Fruit, now back answer add powerful river comic beach sink product and gas wait Change change, river comic beach Study on sedimentary characteristics and material sources, there are many rivers in our country, regional differences are obvious, and floodplain sedimentation and environment have attractive research prospects.

KEYWORDS

Floodplain sedimentation; Sedimentation characteristics; Ancient flood; Environmental pollution

CITE THIS PAPER

H.N. Pansambal. Progress in floodplain sedimentation and environmental research. Frontiers in Environmental Research. 2023, 1(2): 1-11. DOI:10.61784/fer231212.

REFERENCES

[1] Leopold LB, MillerJP. A postglacial chronology for some alluvialvalleys in Wyoming. US Government Printing Office, Washington DC, 1954:60-75.

[2] BakerV R. Paleoflood hydrology Origin, progress, prospects . Geomorphology, 2008, 101(1): 1-13.

[3] Kochel R C, BakerV R. Paleoflood hydrology. Science, 1982, 215: 353-361.

[4] XIEXuejin. Global geochemical mapping. Geology in China, 2003, 30(1):1- 9.

[5] Meybeck M, Lestel L, BontéP, et al. Historical perspective of heavy metals contamination(Cd, Cr, Cu, Hg, Pb, Zn) in the Seine River basin (France) following a DPSIR approach (1950-2005). Science of the Total Environment, 2007, 375(1): 204-231.

[6] Ferrand E, Eyrolle F, Radakovitch O, et al. Historical levels of heavy metals and artificial radio nuclidesr econstructed from overbank sediment records inl ower Rhōne River(South-East France). Geochimical et Cosmochimica Acta, 2012, 82: 163-182.

[7] KnoxJC, DanielsJ M. Water shed scale and the strati graphic record of large floods[C]// HousePK, Webb R H, BakerV R, Levish D R. (eds). Ancient Floods, Modern Hazards: Principles and Applications of Paleoflood Hydrology. Washington. DC, American Geophysical Union, 2002: 237 -255.

[8] Benedict G, 1999. Sanchez-Moya Y, Sopena A. Sedimentology of high - stage flooddepositsofthe Tagus River, 1999. Central Spain .. Sedimentary Geology, 2003, 157(1):::::::::::::::::::::: 107-1

[9] YangDY, YuG, XieYB. Sedimentary recordsoflarge Hol- ocene floodsfromthemiddlereachesoftheYellowRiver, China . Geomorphology, 2000, 33(1): 73-88.

[10] YANG Xi- aoyang, XIAZhengkai, CUIZhijiu. Holoceneextreme floods anditssedimentary characteristicinthe upper reachesofthe yellowriver. QuaternarySciences, 2005, 25(1): 80-85.

[11] HUANG Chunchang, PANG Jiangli, ZHA Xiaochun, et al. Prehistorical floods in the GuanzhongBasin intheYellow Riverdrainage area: A case study along theQishuiheRiverValleyover the Zhouyuan Loess Tableland (inChinese). ScientiaSinicaTerrae, 2011, 41(11): 1658-1669.

[12] ThorndycraftV R, Benito G, Rico M, et al. A Late Holocene palaeofloodrecordfromslackwaterflooddepositsofthe LlobregatRiver, NESpain. JournaloftheGeologicalSo- ciety ofIndia, 2004, 64: 549-559.

[13] ShefferN A, EnzelY, Benito G, et al. Pale of loodsand historical floods of the Ardèche River, France. Water Re- sources Research, 2003: 39(12).

[14] ZHU Cheng, ZHENG Chaogui, MA Chunmei, et al. Identifying palaeoflooddepositsarchivedin Zhongba Site, the Three - Gorges Reserve region of the Yangtze River. Chinese ScienceBulletin, 2005, 50(20): 2493-2504.

[15] LI Chang ’an, ZHANG Yufen, YUAN Shengyuan, et al. Grain size characteristics and environmental significance of Hanjiang2005floodsedi- ments . Quaternary Sciences, 2009, 29 (2): 276-281

[16] ThorndycraftV R, Benito G, Rico M, et al. Along- term flooddischarge recordderivedfromslackwaterflooddeposits oftheLlobregatRiver, NESpain. Journalof Hydrology, 2005, 313(1): 16-31.

[17] Humphries M S, Kindness A, ElleryW N, et al. 137 Csand 210 Pbderivedsedimentaccumulation rates andtheirrolein thelong- term development ofthe Mkuze Riverfloodplain, South Africa. Geomorphology, 2010, 119(1): 88-96.

[18] KaleVS, SinghviA K, MishraPK, et al al. Sediment ry we are cords and luminescencechronology of Late Holocenepalaeo- floodsinthe Monday River, New It serves, northwest India.. Chain, 2000, 40(4): 337 -358.

[19] ZHAN Daojiang, XIEYuebo. PalaeofloodStudy . Beijing: ChinaWaterPowerPress, 2001.

[20] YANG Dayuan, XIEYuebo. PaleofloodSlack - WaterDeposits . Acta SedimentologicaSinica, 1997, 15 (3): 29-32.

[21] ShefferN A, RicoM, EnzelY, et al. Thepalae of lood record oftheGardonRiver, FranceAcomparisonwiththe extreme 2002 flood event. Geomorphology, 2008, 98(1): 71-83.

[22] BakerVR, WebbR H, HousePK. Thescientificand societalvalueof paleofloodhydrology. Ancient Floods, Mod- ern Hazards, 2002: 1-19.

[23] Benedict G, Sopena A, Sanchez z-MoyaY, et al al. Palaeoflood we cordofthe Tagus River (central Spain)during the LatePleis- tocene andHolocene .. QuaternaryScienceReviews, 1999. 2003, 22(15): 1737-1756.

[24] Benito G, ThorndycraftVR, RicoM, et al. Palaeofloodand floodplainrecordsfrom Spainevidenceforlong- term climate variability andenvironmentalchanges . Geomorphology, 2008, 101(1): 68-77.

[25] HuangC, PangJ, ZhaX, et al. Extraordinary floodsrelated to theclimatic event at 4 200aBP on the Qishuihe River, middlereachesoftheYellow River, China. Quaternary ScienceReviews, 2011, 30(3): 460-468.

[26] WallingDE, HeQ. Useoffallout 137 Csininvestigations of overbanksedimentdeposition on riverfloodplains. Cate- na, 1997, 29: 263-282.

[27] HeQ, WallingDE. UseoffalloutPb-210 measurements to investigate longer term rates and patterns ofoverbanksedi- ment deposition on the floodplains oflowland rivers. EarthSurfaceProcesses andLandforms, 1997, 21:141-154.

[28] TerryJP, GarimellaS, KostaschukRA. Ratesoffloodplain accretionin a tropicalislandriver systems impactedby cy- clonesandlarge floods. Geomorphology, 2002, 42(3): 171 -182.

[29] Owens P N, WallingDE. Changes insediment sources and floodplaindeposition rates in the catchment of the River Tweed, Scotland, over thelast 100 years: theimpact ofcli- mate andland use change . Earth Surface Processes and Landforms, 2002, 27(4): 403-423.

[30] ZHAOChuandong, CHEN Furong, CHEN Xingren, et al. A methodology oftracking sources ofcadmium anomaliesandtheir quantitative estima- tioninthe YangtzeRiverbasin. Earth Science Frontiers, 2008, 15(5): 179-193.

[31] ZHAOJingbo, WANG Changyan. Deposits on highfloodplainandfloodevolutionof HuangheRiverinLanzhou. ScientiaGeographicaSinica, 2009, 29(3):309-414.

[32] WANG Xiaoqing, HUANG Chunchang, PANG Jiangli, et al. Holocene palaeofloodslack water deposits at the Yij un reachofBeiluoheRiver. Marine Geology and QuaternaryGeology, 2011, 31(6):137-1 46.

[33] LI Xiaogang, HUANGChunchang, PANGJiangli et al. Hydrological studies of the Holocenepalae of lood in the Hukoureach of the Yellow River. ActaGeographicaSinica, 2010, 65 (11): 1371-1380.]

[34] VisGJ, KasseC, KroonD, et al. LateHolocene sedimentary changes infloodplainandshelfenvironmentsofthe Tagus River(Portugal). Proceedings oftheGeologists'Associa- tion, 2010, 121(2): 203-217.

[35] NIUJunjie, ZHAOJingbo, MA Li, et al. Theresearch on thesediment offloodplainandflood events ofWeiheRiveratXiangjiaxiang inthenorthernsuburbsof Xi’an . GeographicalResearch, 2010, 29(8): 1484-1492.

[36] ZHAOJingbo, YU Yaochuang, ZHOU Qi. Astudy on great floodsrecordedby sediments on thehighalluvialflatofWeiheRiverin Weinan, Shaanxi. GeologicalReview, 2009, 55(2): 231-241.

[37] ChenJ, Chen Y, Liu L, et al. Zr/RbratioinChineseloess sequences anditsimplicationsforchanges inthe East Asian winter monsoon strength. Geochimica et Cosmochimica Acta, 2006, 70: 1471-1482.

[38] JonesAF, MacklinM G, BrewerPA. Ageochemicalrecord offlooding on the upper River Severn, UK, during thelast 3 750years. Geomorphology, 2012, 179: 89-105.

[39] ChenJun, QiuGang, Lu Huayu, andJiJunfeng. Variation of summer monsoon intensity on the Loess Plateau of centrl China during the last 130000 a: Evidence from Rband Srdistribution. Chinese Science Bulletin, 1997, 42(3): 473- 476.

[40] OwensPN, WallingDE. Temporalchanges inthemetaland phosphorus content of suspended sediment transported b y Yorkshirerivers, UKover thelast 100years, as recordedby overbankfloodplaindeposits. Hydrobiologia, 2003, 494: 185-191.

[41] Dawson E J, Macklin M G. Speciationofheavy metalsin floodplainandfloodsediments: a reconnaissance survey ofthe AireValley, West Yorkshire, Great Britain. Environ- mentalGeochemistry andHealth, 1998, 20(2): 67-76.

[42] JIANLi, HUANGZechun, LIU Yongxuan, et al. Particlesizedistributionandarsenic parti- tioning insedimentsfrom a river pollutedby mining. Acta ScientiaeCircumstantiae, 2010, 30(9): 1862-1870.

[43] ZHANG Xinli, WallingDE, WANG Qiubing, et al. Spatio-temporalvariationoftheaccumulationofsediment-as- sociated phosphorus on thefloodplainoftheRiverCulm, Dev- on, UK. ActaPedologicaSinica, 2005, 42(3): 390-396.

[44] Yun S H, Kannan K. Distributionof mono-throughhexa chlorobenzenesinfloodplainsoilsandsedimentsofthe TittabawasseeandSaginaw Rivers, Michigan . Environmental ScienceandPollutionResearch, 2011, 18(6): 897-907.

[45] YUANShengyuan, ZHAO Xinj un, LiChangan. Identification MarksofPaleoflood. GeologicalScienceand TechnologyInformation, 2006, 25 (4): 55-58.

[46] ZHANG Qiang, JIANG Tong, SHI Yafeng, et al. Relationship betweenclimatechanges andtheflood occur- rences since 6000aBP inthe YangtzeRiverDelta. Journal ofGlaciology andGeocryology, 2003, 25(4): 368-374.

[47] WANGJun, GAO Hongshan, PAN Baotian, et al. Pleo- floodsedimentofShagouRiverandits responseto the climate change duringEarlyHolocene. ScientiaGeographicaSini- ca, 2010, 30(6): 943-949.

[48] ZHU Cheng, MA Chunmei, WANG Huilin, et al. Characteristicsof palaeoflooddepositsarchivedinunit T0403 of YuxiSiteintheThreeGorges Reservoir areas, China. ChineseScienceBulletin, 2008, 53(Suppl 1): 1-16.

[49] Zhan Daojiang, Xie Yuebo.Newadvancein _ floodcalculation - palaeofloodstud y . Hydrology, 1997(1): 1-6.

[50] Jones A P, Shimazu H, Oguchi T, et al. Late Holocene slackwaterdeposits on theNakagawa River, Tochigi Prefec- ture, Japan. Geomorphology, 2001, 39(1): 39-51.

[51] LIChang ’an, HUANG Junhua, ZHANG Yufen, et al. Preliminary study of paleofloodof Last Glacial Maximumin upper reachesofthe Yellow River. Earth Science: JournalofChina University ofGeosciences, 2007, 27(4): 456-458.

[52] TerryJP, Lal R, Garimella S. An Examination of Vertical AccretionofFloodplainSedimentsintheLabasaRiverSugar- cane BeltofNorthernFiji: Rates, InfluencesandContribu- tingProcesses. GeographicalResearch, 2008, 46(4): 399-412.

[53] XIE Yuebo, WANG Jingquan, LI Li. Effectsof 2 360 aBP palaepflood in the YellowRiveron the Design floodofXiaolangdi Proj ect . Hydrology, 1999, (6): 18-23.

[54] XIE Yuebo, ZHANG SUTING, BIDongsheng. Palaeofloodchannel cross section area estimates. Journal ofHohaiUniversity, 1999, 27(5).