Abstract
In this chapter sediment discharge and the clogging rate are analysed in order to estimate the lifespan of Cuejdel Lake. The silting processes were identified through indirect calculation methods of soil erosion (USLE) and through geo-physical investigations (direct methods). Based on the indirect methodology of alluvial budget, the result indicates for the catchment area an alluvial production of 3288.5 m3/year (3.02 t/ha/year), in 23 years reaching ca. 75,635.93 m3. From the direct investigation methods, we mention the ground-penetrating radar (GPR) technology, a geo-physical tool accepted long time ago in scientific practice, but unfortunately, shortly used in limnological studies. The bathymetric measurements were concretized by the reconstruction of flooded valley and the achievement of the map of thickness sediments accumulated in the lake basin. In the present time, the water volume was reduced with 297,654.77 m3, from which 103,988.87 m3 were replaced by sediment deposits. The sediment thickness is between 0.1 and 3.6 m. The thickness class 0.1–1.0 m corresponds to 8.552 ha (60.7%) from the lake bottom, 1.0–2.0 m corresponds to 4.676 ha (33.32%), and the thickness class >2.01 m covers the rest of 8326.5 m2 (5.93%). The clogging thickness rate is between 1 and 16 cm/year which means a medium value of 4521.26 m3/year. This value, related to the catchment basin (8.94 km2) and to an effluence rate of 33%, indicates a medium production of sediments—4.33 t/ha/year.
Access this chapter
Tax calculation will be finalised at checkout
Purchases are for personal use only
References
Arghiriade C (1977) Rolul hidrologic al pădurii. Ceres Publishing, Bucharest
Banks WSL, Johnson CD (2011) Collection, processing, and interpretation of ground-penetrating radar data to determine sediment thickness at selected location in deep Creek Lake, Garrett County, Maryland. US Geol Survey–Scientific Investigations Report 2011–5223, Reston, Virginia
Bristow CS, Jol HM (2003) An introduction to ground penetrating radar (GPR) in sediments. In: Bristow CS, Jol HM (eds) Ground penetrating radar in sediments. SP Geol Soc, London 211:1–7
Bryan S, Jeffrey PD (2006) The influence of seasonal precipitation and temperature regimes on lake levels in the northeastern United States during the Holocene. Quatern Res 65:44–56
Buynevich IV, Fitzgerald DM (2003) High-resolution subsurface (GPR) imaging and sedimentology of coastal ponds, Maine, USA: implications for Holocene back-barrier evolution. J Sediment Res 73(4):559–571
Charlie SB, Harry MJ (2003) An introduction to ground penetrating radar (GPR) in sediments. Geol Soc Bull, SP London 211:1–7
Conyers LB (2004) Ground-penetrating radar for archaeology. Alta Mira Press, Walnut Creek
Dagenbach A, Buchner JS, Klenk P, Roth K (2013) Identifying a parameterisation of the soil water retention curve from on-ground GPR measurements. Hydrol Earth Syst Sci 17:611–618
Denziman C, Brevik EC, Doolittle J (2010) Ground-penetrating radar investigation of a rapidly developed small island in a lake in southern Georgia, USA. J Cave and Karst Stud 72(2):94–99
Derald GS, Harry MJ (1995) Ground penetrating radar: antenna frequencies and maximum probable depths of penetration in quaternary sediments. J App Geophys 33:93–100
Diaconu C (1992) Probleme de metodica determinării curbelor teoretice ale probabilităţilor de depăşire (asigurare) în hidrologie. Hidrotehnica–Extras 37(4–5), Bucharest
Elliot JG, Gellis AC, Aby SC (1999) Evolution of arroyos: incised channel of the southwestern United States. In: Simon A (ed) Darby SE. Incised River Channels, Wiley, pp 153–185
Gabbi J, Farinotti D, Bauder A, Maurer H (2012) Ice volume distribution and implications on runoff projections in a glacierized catchment. Hydrol Earth Syst Sci 16:4543–4556
Ichim I (1986) Sistemul aluviunilor. In: Received of 1st Symposium–Provenienţa şi efluenţa aluviunilor, 5–96 November 1986, 1:1–31, Piatra Neamţ
Ichim I, Rădoane N, Rădoane M, Grasu C, Miclăuş C (1998) Dinamica sedimentelor. Aplicaţie la râul Putna-Vrancea. Technical Publishing, Bucharest
McClymont AF, Hayashi M, Bentley LR, Muir D, Ernst E (2010) Groundwater flow and storage within an alpine meadow-talus complex. Hydrol Earth Syst Sci 14:859–872
Mihu–Pintilie A, Romanescu G (2011) Morphometric and morphological suitability of the relief from the Crucii (Cuejdel) Lake basin (Stânişoarei Mountains). In: Pandi G, Moldovan F (eds) Proceedings of the air and water components of the environment, Babeș–Bolyai University, Cluj, 18–19 March 2011, vol 1, pp 305–313
Mihu-Pintilie A, Romanescu G, Stoleriu CC, Nicu IC, Asăndulesei A, Schmaltz E (2014a) Natural dam lakes from Cuejdiu watershed (Stânișoarei Mountains)—Non–invasive methods used for bathymetric maps. In: In: Gâştescu P, Marszelewski W, Breţcan P (eds) Proceedings conference of the water resources and wetlands, Tulcea, 11–13 September 2014, vol 1, pp 130–137
Mihu-Pintilie A, Romanescu G, Stoleriu C (2014b) The seasonal changes of the temperature, pH and dissolved oxygen in the Cuejdel Lake, Romania. Carpat J Earth Environ Sci 9(2):113–123
Mihu-Pintilie A, Paiu M, Breabăn IG, Romanescu G (2014c) Status of water quality in Cuejdi hydrographic basin from Eastern Carpathian, Romania. In: SGEM–proceedings of the 14th international multidisciplinary scientific geoconferences–hydrology and water resources, 18–24 June, Albena, vol 14, no 1, pp 639–646
Mihu-Pintilie A, Asăndulesei A, Nicu IC, Stoleriu CC, Romanescu G (2016) Using GPR for assessing the volume of sediments from the largest natural dam lake of the Eastern Carpathians: Cuejdel Lake, Romania. Environ Earth Sci 75:710. https://doi.org/10.1007/s12665-016-5537-1
Monnier S, Kinnard C, Surazakov A, Bossy W (2014) Geomorphology, internal structure, and successive development of a glacier foreland in the semiarid Chilean Andes (Cerro Tapado, upper Elqui Valley, 30° 08′S, 69° 55′W). Geomorphology 207:126–140
Moorman BJ, Michel FA (1997) Bathymetric mapping and sub-bottom profiling through lake ice with ground-penetrating radar. J Paleolimnology 18:61–73
Moțoc M, Stănescu P, Taloescu I (1979) Actual conceptions regarding erosional phenomenon and it control. Inst Soil Sci Agrochemistry, Agriculture Library, Bucharest
Ndiaye M, Clerc N, Gorin G, Girardclos S, Fiore J (2014) Lake Neuchâtel (Switzerland) seismic stratigraphic record points to the simultaneous Würmian deglaciation of the Rhône Glacier and Jura Ice Cap. Quat Sci Rev 85:1–19
Nicu IC (2013) Analiza riscurilor hidrogeomorfologice care afectează siturile arheologice eneolitice din bazinul hidrografic Valea Oii (Bahlui)–Studii de caz. Alexandru Ioan Cuza University of Iaşi, Disertation
Pan X, Zhang J, Huang P, Roth K (2012) Estimating field-scale soil water dynamics at a heterogeneous site using multi-channel GPR. Hydrol Earth Syst Sci 16:4361–4372
Plado J, Sibul I, Mustasaar M, Jõeleht A (2011) Ground-penetrating radar study of the Rahivere peat bog, eastern Estonian. Estonian J Earth Sci 60:31–42
Proulx-Mclnnis S, St-Hilaire A, Rousseau AN, Jutras S (2013) A review of ground-penetrating radar studies related to peatland stratigraphy with a case study on the determination of peat thickness in a northern boreal fen in Quebec, Canada. Progress in Physical Geography 37(6):767–786
Rădoane N (2002) Un nou lac de baraj natural în bazinul Bistriţei Moldoveneşti-Lacul Cuejdel. Stud Cerc Geograph 49:76–82
Reynolds JM (2011) An Introduction to Applied and Environmental Geophysics–2nd Edition. Wiley Blackwell
Sass O, Krautblatter M, Morche D (2007) Rapid lake infill following major rockfall (bergsturz) events revealed by ground-penetrating radar (GPR) measurements, Reintal, German Alps. The Holocene 17(7):965–976
Schwamborn GJ, Dix JK, Bull JM, Rachold V (2002) High-resolution seismic and ground penetrating radar-geophysical profiling of a Thermokarst Lake in the Western Lena Delta, Northern Siberia. Permafrost Periglac Process 13:259–269
Shuman B, Donnelly JP (2006) The influence of seasonal precipitation and temperature regimes on lake levels in the northeastern United States during the Holocene. Quat Res 65:44–56
Smith DG, Jol HM (1995) Ground penetrating radar: antenna frequencies and maximum probable depths of penetration in quaternary sediments. J Appl Geophys 33:93–100
Stoleriu CC, Romanescu G, Romanescu AM, Mihu-Pintilie A (2015) Morpho-bathymetrical conditions and the silting rate in Stanca-Costesti reservoir (Romania). Wulfenia J 22(2):451–470
Syvitski JPM, Milliman J (2007) Geology, geography, and humans battle for dominance over the delivery of fluvial sediment to the coastal ocean. J Geology 115:1–19
Surdeanu V (1998) Geografia terenurilor degradate–Alunecări de teren. Cluj University Press, Cluj-Napoca
Vanmaercke M, Obreja F, Poesen J (2014) Seismic control on contemporary sediment export in the Siret river catchment, Romania. Geomorphology 216:247–262
Author information
Authors and Affiliations
Corresponding author
Rights and permissions
Copyright information
© 2018 Springer International Publishing AG, part of Springer Nature
About this chapter
Cite this chapter
Mihu-Pintilie, A. (2018). Nature of Lacustrine Sediments and Clogging Rate. In: Natural Dam Lake Cuejdel in the Stânişoarei Mountains, Eastern Carpathians. Springer, Cham. https://doi.org/10.1007/978-3-319-77213-4_6
Download citation
DOI: https://doi.org/10.1007/978-3-319-77213-4_6
Published:
Publisher Name: Springer, Cham
Print ISBN: 978-3-319-77212-7
Online ISBN: 978-3-319-77213-4
eBook Packages: Earth and Environmental ScienceEarth and Environmental Science (R0)