Karst hydrogeology/hydrology of dinaric chain and isles
详细信息    查看全文
  • 作者:Ognjen Bonacci
  • 关键词:Karst hydrogeology ; Karst hydrology ; Karst spring ; Karst lake ; Karst island ; Dinaric karst
  • 刊名:Environmental Earth Sciences
  • 出版年:2015
  • 出版时间:July 2015
  • 年:2015
  • 卷:74
  • 期:1
  • 页码:37-55
  • 全文大小:4,703 KB
  • 参考文献:Babinka S (2007) Multi-tracer study of karst waters and lake sediments in Croatia and Bosnia—Herzegovina: Plitvice Lakes, National Park and Biha? area. Ph.D. Thesis, Rheinischen Friedrich Wilhelms Universit?t, Bonn
    Benac ?, Rubini? J, O?ani? N (2003) The origin and evolution of coastal and submarine springs in Bakar Bay. Acta Carsologica 32(1):157-71
    Biondi? B, Biondi? R, Mea?ki H (2010) The conceptual hydrogeological model of the Plitvice Lakes. Geol Croat 63(2):195-06
    Bonacci O (1987) Karst hydrology with special references to Dinaric karst. Springer Verlag, Berlin
    Bonacci O (1993) The Vrana Lake hydrology (island of Cres—Croatia). Water Res Bull 29(3):407-14View Article
    Bonacci O (1995) Ground water behaviour in karst: example of the Ombla Spring (Croatia). J Hydrol 165(1-):113-34View Article
    Bonacci O (1999) Water circulation in karst and determination of catchment areas: example of the River Zrmanja. Hydrol Sci J 44(3):373-86View Article
    Bonacci O (2001) Analysis of the maximum discharge of karst springs. Hydrogeol J 9(4):328-38View Article
    Bonacci O (2011) Hidrolo?ka analiza odvo?enja vode iz kr?kog izvora rijeke Jadro. Hrvatske Vode 20(79-0):37-2 (Croatian)
    Bonacci O (2012) Increase of mean annual surface air temperature in the Western Balkans during last 30?years. Vodoprivreda 44(255-57):75-9
    Bonacci O (2013) Zabrinjavaju?i hidrolo?ki trendovi na slivu Plitvi?kih jezera. Hrvatske Vode 21(84):137-45 (Croatian)
    Bonacci O, Andri? I (2008) Sinking karst rivers hydrology: case of the Lika and Gacka (Croatia). Acta Carsologica 37(2-):185-96
    Bonacci O, Andri? I (2010) Impact of inter-basin water transfer and reservoir operation on a karst open streamflow hydrological regime: an example from the Dinaric karst (Croatia). Hydrol Process 24(26):3852-863View Article
    Bonacci O, Roje-Bonacci T (1997) Sea water intrusion in coastal karst springs: example of the Bla? Spring. Hydrol Sci J 42(1):89-00View Article
    Bonacci O, Roje-Bonacci T (2003) The influence of hydroelectrical development on the flow regime of the karstic river Cetina. Hydrol Process 17(1):1-5View Article
    Bonacci O, Roje-Bonacci T (2008) Water losses from the Ri?ica reservoir built in the Dinaric karst. Eng Geol 99(3-):121-27View Article
    Bonacci O, ?ivaljevi? R (1993) Hydrological explanation of the flow in karst: example of the Crnojevi?a spring. J Hydrol 146:405-19View Article
    Bonacci O, Juki? D, Ljubenkov I (2006) Definition of catchment area in karst: case of the rivers Kr?i? and Krka, Croatia. Hydrol Sci J 51(4):682-99View Article
    Bonacci O, Ljubenkov I, Knezi? S (2012) The water on a small karst island of Kor?ula (Croatia) as an example. Environ Earth Sci 66(5):1345-347View Article
    Bonacci O, ?eljkovi? I, Gali? A (2013) Karst rivers-particularity: an example from Dinaric karst (Croatia/Bosnia and Herzegovina). Environ Earth Sci 70(2):963-74View Article
    Bonacci O, Andri? I, Yamashiki Y (2014) Hydrology of Blue Lake in the Dinaric karst. Hydrol Process 28(4):1890-898View Article
    Breznik M (1998) Storage reservoirs and deep wells in karst regions. A.A.Balkema, Rotterdam
    Cooper HH (1959) A hypothesis concerning the dynamic balance of fresh water and salt water in a coastal aquifer. J Geophys Res 64:461-67View Article
    Cviji? J (1893) Das Karstph?nomen. Pencks Geogr Abh 5(3):217-30 (German)
    Deni?-Juki? V, Juki? D (2003) Composite transfer functions for karst aquifers. J Hydrol 274(1-):80-4View Article
    Duplan?i?-Leder T, Ujevi? T, ?ala M (2004) Coastline lengths and areas of islands in the Croatian part if the Adriatic Sea determined from the topographic maps at scale of 1:25,000. Geoadria 9(1):5-2
    Fairbanks RG (1989) A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342:637-42View Article
    Falkland A (ed) (1991) Hydrology and water resources of small islands: a practical guide. UNESCO, Paris
    Gabrov?ek F, Turk J (2011) Water temperature as a natural tracer of groundwater in karst: the case of the Pivka and Unica Rivers. In: Knez M, Petri? M, Slabe T (eds) Karstology and development challenges on karst I. Carsologica 12, pp 38-6
    Gams I (1974) Kras. Zgodovinski, naravoslovni in geografski oris. Slovenska Matica, Ljubljana (Slovenian)
    Ghyben WB (1888) Nota in verband met de voorgenomen putboring nabij Amsterdam, vol 21. Tijdschrift Let Koninklijk Instituut van Ingenieurs, The Hague, pp 8-2 (Dutch)
    Gospodari? R, Habi? P (eds) (1976) Underground water tracing—Investigations in Slovenia 1972-975. Institute for Karst Research SAZU, Ljubljana
    Hertelendi E, Svingor E, Rank D, Futo I (1995) Isotope investigation of lake Vrana and springs of Kvarner area. In: Proceedings of the first Croatian geological congress, vol 1. Opatija, pp 201-05
    Herzberg A (1901) Die Wassergersorgung einiger Nordseeb?der. Journal für Gasbeleucht
  • 作者单位:Ognjen Bonacci (1)

    1. Faculty of Civil Engineering, Architecture and Geodesy, Split University, Matice hrvatske 15, 21000, Split, Croatia
  • 刊物类别:Earth and Environmental Science
  • 刊物主题:None Assigned
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1866-6299
文摘
This paper gives a comprehensive explanation of the hydrogeological and hydrological characteristics of different water occurrence, which exists in the extremely complex Dinaric karst system. The area and boundaries of the Dinaric karst have never been precisely determined. It covers about 60,000?km2 stretching the length of the eastern coast of the Adriatic Sea, from the Bay of Trieste in the north, to the Drim River basin in the south, and the Western Morava River valley in the east. Due to very high infiltration rates, overland and surface flows are rare in comparison with non-karst terrains. The Dinaric karst is an extremely heterogeneous medium which can be explained only by the use of a great number of measurements points and by continuously monitoring and measuring different parameters. The hydrogeological and hydrological regime of all water phenomena in the Dinaric karst depends mostly upon the interaction between groundwater and surface water. The dominant flow of the groundwater contained in the Dinaric karst is towards the Adriatic Sea through rivers and many permanent and intermittent coastal and submarine springs. The paper presents many examples of karst water phenomena from the Dinaric karst: (1) springs (Jadro, Ombla and Crnojevi?a Springs); (2) open streamflows (Ljubljanica, Pazin?ica, Dobra, Lika, Gacka, Krka, Zrmanja and Cetina Rivers); (3) lakes and wetlands (Cerknica, Vrana, Plitvice, Vransko, Red and Blue Lakes); and (4) coastal and island karst (Bra? Island).

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700