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Journal articles on the topic 'Karst hydrogeology'

Author: Grafiati

Published: 4 June 2021

Last updated: 11 February 2022

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1

Hess, John W. "Methods in Karst Hydrogeology." Ground Water 46, no. 2 (2008): 172. http://dx.doi.org/10.1111/j.1745-6584.2007.00429.x.

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2

Edgell, H. S. "Karst and hydrogeology of Lebanon." Carbonates and Evaporites 12, no. 2 (1997): 220–35. http://dx.doi.org/10.1007/bf03175419.

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3

Drew, D. P. "Hydrogeology of lowland karst in Ireland." Quarterly Journal of Engineering Geology and Hydrogeology 41, no. 1 (2008): 61–72. http://dx.doi.org/10.1144/1470-9236/07-027.

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4

Andreo, Bartolomé. "Introductory editorial: advances in karst hydrogeology." Environmental Earth Sciences 65, no. 8 (2012): 2219–20. http://dx.doi.org/10.1007/s12665-012-1621-3.

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5

Özler, Murat. "Karst hydrogeology of Kusluk-Dilmetas karst springs, Van-Eastern Turkey." Environmental Geology 41, no. 3-4 (2001): 257–68. http://dx.doi.org/10.1007/s002540100401.

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6

Goldscheider, Nico, Joe Meiman, Michiel Pronk, and Christopher Smart. "Tracer tests in karst hydrogeology and speleology." International Journal of Speleology 37, no. 1 (2008): 27–40. http://dx.doi.org/10.5038/1827-806x.37.1.3.

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7

Fiorillo, Francesco, and Zoran Stevanović. "Introductory editorial thematic issue: Mediterranean karst hydrogeology." Environmental Earth Sciences 74, no. 1 (2015): 1–3. http://dx.doi.org/10.1007/s12665-015-4548-7.

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8

Gröbner, Katharina, Wolfgang Gadermayr, Giorgio Höfer-Öllinger, Harald Huemer, and Christoph Spötl. "Karst hydrogeology of Lamprechtsofen (Leoganger Steinberge, Salzburg)." Austrian Journal of Earth Sciences 112, no. 1 (2019): 50–61. http://dx.doi.org/10.17738/ajes.2019.0004.

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AbstractThe Leoganger Steinberge are a heavily karstified massif largely composed of Dachstein dolomite and limestone hosting the deepest through-trip cave in the world, Lamprechtsofen, whose frontal parts are developed as a show cave. Many parts of this 60 km-long and 1724 m-deep system are hydrologically active. 1.5 km behind the lower cave entrance Grüntopf stream and Kneippklamm stream merge to form the main cave stream. Another underground stream, Stainerhallen stream, flows through the eponymous hall of the show cave. Since 2007 water temperature, electrical conductivity and water level

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9

LaMoreaux, Philip E., and Jim LaMoreaux. "Karst: the foundation for concepts in hydrogeology." Environmental Geology 51, no. 5 (2006): 685–88. http://dx.doi.org/10.1007/s00254-006-0378-y.

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10

Fiorillo, Francesco, and Peter Malik. "Hydraulic Behavior of Karst Aquifers." Water 11, no. 8 (2019): 1563. http://dx.doi.org/10.3390/w11081563.

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The objective of this Special Issue, “Hydraulic Behavior of Karst Aquifers”, is to focus on recent advances in karst hydrogeology in different areas of the world, focusing on topics dealing with the peculiar characteristics of karst aquifers. In particular, thirteen peer-reviewed articles were collected, focusing on hydraulic aspects and their relationship with geological features, geochemical and bacteriological aspects, tunneling and engineering mining inrush, and forecasting water resources and drought occurrences. Overall, these contributions describe several aspects of karst aquifers and

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11

Troester, Joseph W., and John E. Moore. "Karst hydrogeology in the United States of America." Episodes 12, no. 3 (1989): 172–78. http://dx.doi.org/10.18814/epiiugs/1989/v12i3/004.

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12

Bonacci, Ognjen. "Karst hydrogeology/hydrology of dinaric chain and isles." Environmental Earth Sciences 74, no. 1 (2014): 37–55. http://dx.doi.org/10.1007/s12665-014-3677-8.

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13

Nekouei, Esmaeil, and Mehdi Zarei. "Karst hydrogeology of Karmustadj salt diapir, southern Iran." Carbonates and Evaporites 32, no. 3 (2016): 315–23. http://dx.doi.org/10.1007/s13146-016-0298-1.

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14

Auler, Augusto S., and Zoran Stevanović. "Preface: Five decades of advances in karst hydrogeology." Hydrogeology Journal 29, no. 1 (2021): 1–6. http://dx.doi.org/10.1007/s10040-020-02292-x.

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15

Bosch, Rachel. "Development and implementation of virtual field teaching resources: two karst geomorphology modules and three virtual capstone pathways." Geoscience Communication 4, no. 2 (2021): 329–49. http://dx.doi.org/10.5194/gc-4-329-2021.

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Abstract. During the summer of 2020, many geology field camps were canceled due to the COVID-19 pandemic, including the karst geomorphology field course I was scheduled to co-teach through Western Kentucky University. When the National Association of Geoscience Teachers (NAGT), in collaboration with the International Association for Geoscience Diversity (IAGD), began the project of supporting working groups to create online field experience teaching materials, this presented an opportunity. This paper describes the development of two activities derived from that field camp curriculum that are

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16

Trček, Branka. "Epikarst zone of a karst aquifer – its characteristics and importance in karst hydrogeology." Geologija 45, no. 2 (2002): 573–78. http://dx.doi.org/10.5474/geologija.2002.067.

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17

Epting, J., D. Romanov, P. Huggenberger, and G. Kaufmann. "Integrating field and numerical modeling methods for applied urban karst hydrogeology." Hydrology and Earth System Sciences Discussions 6, no. 2 (2009): 3577–635. http://dx.doi.org/10.5194/hessd-6-3577-2009.

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Abstract. Infrastructures that are constructed on unstable geologic formations are prone to subsidence. Data have been collected in the context of an upgrading project for a highway located beside a river dam that was constructed on gypsum-containing formations. Surface water infiltrates upstream of the dam, circulates through the gravel deposits and into the weathered bedrock around and beneath the dam, and exfiltrates downstream into the river. As a result, an extended weathering zone within the bedrock and preferential flow paths within voids and conduits developed as part of a rapidly evol

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18

Benischke, Ralf. "Review: Advances in the methodology and application of tracing in karst aquifers." Hydrogeology Journal 29, no. 1 (2021): 67–88. http://dx.doi.org/10.1007/s10040-020-02278-9.

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AbstractTracer methods have been widely used in many fields of environmental and natural sciences, and also in human health sciences. In particular, tracers are used in the study of karst hydrogeology, typically focusing on phenomena such as sinkholes, sinking rivers and large karst springs. It is known that tracers have been used since antiquity. The aim of tracer tests has been to investigate underground flow paths, transport processes and water–rock interactions, and to get an insight into the functioning of a karst aquifer. In karst hydrogeology, tracer methods are the most important inves

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19

Field, M. S. "Karst Hydrogeology and Human Activities: Impacts, Consequences, and Implications." Environmental & Engineering Geoscience V, no. 4 (1999): 487–89. http://dx.doi.org/10.2113/gseegeosci.v.4.487.

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20

Ho, H. C. "The role of karst in engineering and environmental geosciences." Solid Earth Discussions 3, no. 1 (2011): 149–58. http://dx.doi.org/10.5194/sed-3-149-2011.

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Abstract. Karst is a unique landform developed by soluble rock. It usually relates to groundwater drainage system, and provides important water resources. Current researches indicate that karst is closely related to the earth system and environmental protection, and it can also create potential natural hazard such as sinkhole flooding and land subsidence in urban area. Its relationship with hydrogeology has also been an important factor for studying water pollution, and nutrient cycles on engineering geosciences and agricultural geology.

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21

Zhu, Qing Qing, Qiang Qiang Miao, and Shu Ping Jiang. "On Karst Water Inrush (Gushing) Geological Environment in Pingyang Tunnel." Applied Mechanics and Materials 580-583 (July 2014): 1008–12. http://dx.doi.org/10.4028/www.scientific.net/amm.580-583.1008.

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According to Pingyang tunnel karst complex groundwater environment ,This paper carried out thorough theoretical analysis and field observation from Pingyang tunnel stratum rock properties, engineering geology, hydrogeology, the surrounding patch, runoff and drainage and the changes of surface water environment, as well as tunnel excavating. The complex formation mechanism has given in the Pingyang tunnel karst water . Some effective references had put forward for the engineering treatment, provided some valuable references for other similar underground engineering construction.

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22

Ho, H. C. "The role of karst in engineering and environmental geosciences." Solid Earth 2, no. 2 (2011): 155–58. http://dx.doi.org/10.5194/se-2-155-2011.

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Abstract. Karst is a unique landform developed by soluble rock. It usually relates to the groundwater drainage system, and provides important water resources. Current researches indicate that karst is closely related to the Earth system and environmental protection, and it can also create potential natural hazards such as sinkhole flooding and land subsidence in urban area. Its relationship with hydrogeology has also been an important factor for studying water pollution and nutrient cycles in engineering geosciences and agricultural geology.

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23

Wang, Yu Shan, Zhi Hua Chen, and Fu Cun Zhang. "Numerical Simulation for Karst Water Drainage of an Iron Mine." Advanced Materials Research 450-451 (January 2012): 486–90. http://dx.doi.org/10.4028/www.scientific.net/amr.450-451.486.

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An iron mine in Fujian that is mining a hydrologically complicated deposit with karst water, faces the problems of high water pressure and unclear inflow. Therefore, it’s imperative to predict mine discharge exactly. The 3D finite element simulation model is established basing exploration data and theoretical analysis results, which gives exact generalization of special hydrogeology elements such as fault zone, karst springs, surface water leakage and chamber for dewatering. At last, the effect of dewatering scheme are evaluated for +300m.

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24

Yao, Guang Hua, Zheng Hua Chen, Chang Peng Tu, Xi Qiong Xiang, and Sheng Xu. "Failure Mode of Karst Water under Inclined Coal Seam Mining in Hilly Area." Advanced Materials Research 599 (November 2012): 732–38. http://dx.doi.org/10.4028/www.scientific.net/amr.599.732.

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Using special hydrogeology survey, groundwater level observation, water pressure test, pit infiltration test, imaging well log technique and Hertz wave CT in the mining subsidence area and its nearby, failure mode of karst water under inclined coal seam mining in hilly area is studied. Contrasted surface infiltration capacity of limestone in 1955 with in 2011, it verifies that aquicludes and aquifers above goaf and near ground are damaged, therefore karst water in different aquifers become a unified water-bearing body. In the mining subsidence area, karst water forms a cone of depression, and

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25

Epting, J., D. Romanov, P. Huggenberger, and G. Kaufmann. "Integrating field and numerical modeling methods for applied urban karst hydrogeology." Hydrology and Earth System Sciences 13, no. 7 (2009): 1163–84. http://dx.doi.org/10.5194/hess-13-1163-2009.

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Abstract. Infrastructures constructed on unstable geologic formations are prone to subsidence. Data have been collected in the context of an upgrading project for a highway located beside a river dam constructed on gypsum-bearing formations. Surface water infiltrates upstream of the dam, circulates through the gravel deposits and into the weathered bedrock around and beneath the dam, and exfiltrates downstream into the river. As a result, an extended weathering zone within the bedrock and preferential flow paths within voids and conduits developed as part of a rapidly evolving karst system. En

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26

Miklós, Rita, László Lénárt, Enikő Darabos, et al. "Karst water resources and their complex utilization in the Bükk Mountains, northeast Hungary: an assessment from a regional hydrogeological perspective." Hydrogeology Journal 28, no. 6 (2020): 2159–72. http://dx.doi.org/10.1007/s10040-020-02168-0.

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Abstract The cold and thermal karst water resources of the Bükk Mountains play a significant role in the hydrogeological setting of northeastern Hungary. Although there is much geological and hydrogeological information available, the regional hydrogeology of the Bükk Mountains had not been described in a standalone study involving all this information. The drinking water supply of the city of Miskolc and some other neighboring cities is based on the cold karst water resources of the Bükk Mountains. The thermal water resources have been getting more important, in terms of balneology and geothe

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27

Onac, Bogdan. "Geochemical Sediments & Landscape; Cave Geology; Karst Hydrogeology and Geomorphology." Studia Universitatis Babes-Bolyai, Geologia 53, no. 1 (2008): 39. http://dx.doi.org/10.5038/1937-8602.53.1.5.

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28

Mueller, Michael. "Karst hydrogeology of the Takaka valley, Golden Bay, northwest Nelson." New Zealand Journal of Geology and Geophysics 34, no. 1 (1991): 11–16. http://dx.doi.org/10.1080/00288306.1991.9514434.

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29

Goldie, Helen. "Book Review: Karst hydrogeology and human activities: consequences and implications." Progress in Physical Geography: Earth and Environment 26, no. 2 (2002): 306–7. http://dx.doi.org/10.1177/030913330202600210.

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30

Baechler, Fred, and Robert Boehner. "Karst geology and hydrogeology of Cape Breton Island, Nova Scotia: an overview." Canadian Journal of Earth Sciences 51, no. 7 (2014): 701–14. http://dx.doi.org/10.1139/cjes-2013-0157.

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Approximately 23% (2700 km2) of Cape Breton Island consists of a wide variety of glaciated bedrock (meta-carbonates, carbonates, and evaporites) that has the potential for karst development. An additional 1100 km2 of such strata have been inundated by post-glacial sea-level rise. There have been three main episodes of karstification. The Island represents a portion of the tectonically ancient, deep crustal, eroded terrain of the Appalachian Orogen, more recently influenced by the interplay of sea-level change, ice sheet stability, transient ice aquifers, climate change, and isostatic rebound.

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31

Di Cicco, Mattia, Tiziana Di Lorenzo, Mattia Iannella, Ilaria Vaccarelli, Diana Maria Paola Galassi, and Barbara Fiasca. "Linking Hydrogeology and Ecology in Karst Landscapes: The Response of Epigean and Obligate Groundwater Copepods (Crustacea: Copepoda)." Water 13, no. 15 (2021): 2106. http://dx.doi.org/10.3390/w13152106.

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Groundwater invertebrate communities in karst landscapes are known to vary in response to multiple environmental factors. This study aims to explore the invertebrate assemblages’ composition of an Apennine karst system in Italy mainly described by the Rio Gamberale surface stream and the Stiffe Cave. The stream sinks into the carbonate rock and predominantly feeds the saturated karst into the cave. For a minor portion, groundwater flows from the epikarst and the perched aquifer within it. The spatial distribution of the species belonging to the selected target group of the Crustacea Copepoda b

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32

Yan, Zhi Wei, Hui Li Liu, Zhi Gan Zhang, and Shui Xin Li. "A New Metal Ore Karst Deposition Form - Case Study for Dolomite Residual Deposit in Dongxiang Copper Mine, Jiangxi Province, China." Advanced Materials Research 838-841 (November 2013): 1830–35. http://dx.doi.org/10.4028/www.scientific.net/amr.838-841.1830.

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The Kcd (Karst colluvium and deluvium) deposit of Dongxiang copper mine had long been considered as a kind of ancient diluvium, alluvium and proluvium in Cretaceous Karst depression. Based on lithology and morphology analysis of Kcd, and further research for regional hydrogeology and hydrogeochemistry, it was considered as a new special Karst deposition form of metal ore in this project. In the oxidation zone of sulfide mineral deposit, Kcd was a deposition mixture of dolomite powder (sand) and eluvium of dolomite wall rock, which were generated by the action of sulfuric acid water on wall roc

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33

Zarei, Mehdi, and Ezatolah Raeisi. "Karst development and hydrogeology of Konarsiah salt diapir, south of Iran." Carbonates and Evaporites 25, no. 3 (2010): 217–29. http://dx.doi.org/10.1007/s13146-010-0027-0.

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34

Dar, Farooq Ahmad, Jerome Perrin, Shakeel Ahmed, and Allu China Narayana. "Review: Carbonate aquifers and future perspectives of karst hydrogeology in India." Hydrogeology Journal 22, no. 7 (2014): 1493–506. http://dx.doi.org/10.1007/s10040-014-1151-z.

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35

E. Marín, Luis, Birgit Steinich, Julia Pacheco, and Oscar A. Escolero. "Hydrogeology of a contaminated sole-source karst aquifer, Mérida, Yucatán, Mexico." Geofísica Internacional 39, no. 4 (2000): 359–65. http://dx.doi.org/10.22201/igeof.00167169p.2000.39.4.246.

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La ciudad de Mérida, Yucatán obtiene su agua potable principalmente de tres campos de pozos localizados en los alrededores de la ciudad. Adicionalmente, existen pozos del sistema de agua potable dentro de la ciudad. Se ha reportado la presencia de plomo, cadmio y cromo excediendo el límite de la Norma de Agua Potable Mexicana en agua del sistema de agua potable. Los siguientes contaminantes orgánicos también han sido detectado en el agua subterránea de la porción sur de la ciudad: TCA, PCE, TCE y CTET. Mérida obtiene aproximadamente 65% de su agua potable del campo de pozos JAPAY-I, el cual ex

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36

Barna, Joshua M., Alan E. Fryar, Le Cao, Benjamin J. Currens, Tao Peng, and Chen Zhu. "Variability in Groundwater Flow and Chemistry in the Houzhai Karst Basin, Guizhou Province, China." Environmental and Engineering Geoscience 26, no. 3 (2020): 273–89. http://dx.doi.org/10.2113/eeg-2306.

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ABSTRACT Understanding how karst aquifers store and transmit water and contaminants is an ongoing problem in hydrogeology. Multiple flow paths and recharge heterogeneity contribute to the complexity of these systems. This study explored karst-conduit connectivity and water-chemistry variability within the Houzhai catchment in Guizhou Province, China. Artificial tracer tests were conducted during both the monsoon and dry seasons to understand temporal variability in connectivity and water velocity between karst features. Multiple flow paths through the catchment were activated during the monsoo

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37

Xeidakis, G. S., A. Torok, S. Skias, and B. Kleb. "ENGINEERING GEOLOGICAL PROBLEMS ASSOCIATED WITH KARST TERRAINS: THEIR INVESTIGATION. MONITORING, AND MITIGATION AND DESIGN OF ENGINEERING STRUCTURES ON KARST TERRAINS." Bulletin of the Geological Society of Greece 36, no. 4 (2004): 1932. http://dx.doi.org/10.12681/bgsg.16679.

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The design and construction of civil engineering structures in karst regions confronts many problems due to unpredictable location, dimensions and geometry of the karst structure and voids. Karst terrain is one of the most intricate grounds to be assessed for civil engineering purposes. Conventional methods of site exploration like desk studies, site reconnaissance, borings, test pits, geophysical techniques, have their advantages and disadvantages; none of them are 100% accurate; therefore they should be used in concert, adapted to each project, the available budget and the undertaken risk. A

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38

Zhou, Chao Yue, Yong Fang, Ya Peng Fu, and Ge Cui. "The Grouting Technology of Large-Section Highway Tunnel in Water-Rich Karst Formations." Advanced Materials Research 838-841 (November 2013): 1441–46. http://dx.doi.org/10.4028/www.scientific.net/amr.838-841.1441.

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It is a challenge to deal with karst in the construction of large cross-section tunnel. Under the background of Shuangbei Highway Tunnel, a new kind of grouting technology is introduced. According to hydrogeology, field tests are carried out to select grouting materials and proportion of mixture. Combined with the project practice, grouting construction technology is discussed such as grouting equipments, grouting parameters, operation technique, grouting ending standards. It has been proved that the technology is effective in tunnel construction.

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39

Abirifard, Mahmoud, Ezzat Raeisi, Mehdi Zarei, et al. "Jahani Salt Diapir, Iran: hydrogeology, karst features and effect on surroundings environment." International Journal of Speleology 46, no. 3 (2017): 445–57. http://dx.doi.org/10.5038/1827-806x.46.3.2133.

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40

Williams, Paul. "The role of the epikarst in karst and cave hydrogeology: a review." International Journal of Speleology 37, no. 1 (2008): 1–10. http://dx.doi.org/10.5038/1827-806x.37.1.1.

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41

Williams, Paul W. "Book Review: Methods in Karst Hydrogeology, Nico Goldscheider and David Drew (eds)." Hydrogeology Journal 17, no. 4 (2008): 1025. http://dx.doi.org/10.1007/s10040-008-0393-z.

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42

Hobbs, P., and N. de Meillon. "Hydrogeology of the Sterkfontein Cave System, Cradle of Humankind, South Africa." South African Journal of Geology 120, no. 3 (2017): 403–20. http://dx.doi.org/10.25131/gssajg.120.3.403.

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Abstract A water level rise of almost 3 m in the space of two years in the Sterkfontein Cave system since late-2009 necessitated the re-routing of the tourist path through the cave to successively higher elevations on three occasions. It also raised concern for a possible association with copious acidic and sulphate-rich mine water drainage from the West Rand Goldfield (a.k.a. Western Basin) starting in early-2010, and the related threat to the UNESCO-inscribed fossil site. Although these circumstances have had little impact on the tourist value of the site, a prognosis of the impact on cave w

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43

Li, Bo, Yan Jun Wu, and Bin Zhao. "Assessment on Sustainability of Groundwater Resources in China Southwestern Karst Mountain Area." Advanced Materials Research 726-731 (August 2013): 3381–84. http://dx.doi.org/10.4028/www.scientific.net/amr.726-731.3381.

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Based on the systematical analysis of hydrogeology, social economy and regional environment, choosing 23 indicators from four aspects of the groundwater resources condition, social economy, the ecological environment, Sustainability assessment system of groundwater resources for southwestern karst mountain area were established. Meanwhile, the weights of the indicators based on AHP were determined, which can reduce the fuzziness of man-made judgments. the sustainability of groundwater resources were evaluated and had a much better result by referring to the Weining area of Guizhou province. Th

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44

Zhang, Zhengxian, Weiping Wang, Shisong Qu, et al. "A New Perspective to Explore the Hydraulic Connectivity of Karst Aquifer System in Jinan Spring Catchment, China." Water 10, no. 10 (2018): 1368. http://dx.doi.org/10.3390/w10101368.

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Investigating the hydraulic connectivity of a complex karst aquifer system is an important research topic for sustainable operation and optimization layout of karst groundwater exploitation and recharge. However, the identification of preferential sites of recharge and exploitation is usually subject to regional hydrogeology conditions and the mechanisms of recharge and exploitation. The conventional research methods of hydraulic connectivity often have some limitations. In this study, we developed an improved grey amplitude relation model to explore the hydraulic connectivity in Jinan spring

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45

Elhatip, H., and G. Günay. "Karst hydrogeology of the Kaş-Kalkan springs along the Mediterranean coast of Turkey." Environmental Geology 36, no. 1-2 (1998): 150–58. http://dx.doi.org/10.1007/s002540050330.

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46

Oraseanu, Iancu, and John Mather. "Karst hydrogeology and origin of thermal waters in the Codru Moma Mountains, Romania." Hydrogeology Journal 8, no. 4 (2000): 379–89. http://dx.doi.org/10.1007/s100400000080.

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47

McCormack, T., Y. O’Connell, E. Daly, L. W. Gill, T. Henry, and M. Perriquet. "Characterisation of karst hydrogeology in Western Ireland using geophysical and hydraulic modelling techniques." Journal of Hydrology: Regional Studies 10 (April 2017): 1–17. http://dx.doi.org/10.1016/j.ejrh.2016.12.083.

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48

Wan, Fei, Peiwen Xu, Peng Zhang, Hongfu Qu, Lihua Wang, and Xuan Zhang. "Quantitative Inversion of Water-Inrush Incidents in Mountain Tunnel beneath a Karst Pit." Advances in Civil Engineering 2021 (July 22, 2021): 1–18. http://dx.doi.org/10.1155/2021/9971944.

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Quantitative inversion of accidents is an important work of finding the cause of accidents and avoiding their recurrence. However, quantitative inversion of accidents is difficult due to the lack and limitation of accidents monitoring information. Focusing on water-inrush incidents of Jiguan Mountain tunnel, this paper proposes a set of workflows to find out the missing conditions and quantitative inversion of accidents by flow analysis and structural safety analysis on the basis of investigating the rain capacity and water outflow in water-inrush incidents. First, hydraulic boundary in water-

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49

Liu, Jian, and Dan Liu. "Evaluation of the Environmental Impact Produced by Xulingguan Tunnel Construction Using an Indicator System." Advanced Materials Research 347-353 (October 2011): 1237–40. http://dx.doi.org/10.4028/www.scientific.net/amr.347-353.1237.

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In order to evaluate the environmental impact of tunnel construction in karst areas, this document establishes an indicator system consisting of physical geography, geology and hydrogeology as well as tunnel engineers and 19 specific indicators, along with grades and standards for assessment. The weight of each factor is determined using analytic hierarchy process, and fuzzy comprehensive evaluation method is adopted to make a comprehensive evaluation. Basing on investigation and documentary, Xulingguan tunnel is taken as an example, and its environmental impact grade is assessed between very

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Herman, Ellen K., Laura Toran, and William B. White. "Clastic sediment transport and storage in fluviokarst aquifers: an essential component of karst hydrogeology." Carbonates and Evaporites 27, no. 3-4 (2012): 211–41. http://dx.doi.org/10.1007/s13146-012-0112-7.

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