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Relevant bibliographies by topics / Karst Environments

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Academic literature on the topic 'Karst Environments'

Author: Grafiati

Published: 4 June 2021

Last updated: 8 February 2022

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Journal articles on the topic "Karst Environments"

1

Dandurand, Grégory. "Book review: Preserving karst environments and karst caves. Karst dynamics, environments, usage and restauration: Towards an international karst preservation system." Géomorphologie : relief, processus, environnement 24, no. 2 (July 15, 2018): 185–86. http://dx.doi.org/10.4000/geomorphologie.11964.

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Dandurand, Grégory. "Compte rendu de lecture : Preserving karst environments and karst caves. Karst dynamics, environments, usage and restauration: Towards an international karst preservation system." Géomorphologie : relief, processus, environnement 24, no. 2 (July 15, 2018): 185–86. http://dx.doi.org/10.4000/geomorphologie.11963.

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Dan, Yong, Liangbiao Lin, Bin Liang, Qingyu Zhang, Yu Yu, Jianwen Cao, and Jingrui Li. "Eogenetic Karst Control of Carbonate Reservoirs during a Transient Exposure: A Case Study of the Ordovician Yingshan Formation in the Northern Slope of the Tazhong Uplift, Tarim Basin, China." Minerals 8, no. 8 (August 9, 2018): 345. http://dx.doi.org/10.3390/min8080345.

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The Tazhong area of the Tarim Basin contains abundant oil and gas resources in Ordovician carbonate rocks, especially in the karst pores and caves of the Yingshan Formation. Research has indicated that the Yingshan Formation underwent a 7–11 Ma exposure during the middle Caledonian Period, resulting in large-scale karst pores and caves. However, the continental freshwater karst model cannot adequately explain the origin and distribution of karst pores and caves. In order to develop a more accurate karst model to guide petroleum exploration in the region, we analyzed the karst morphology, cave development statistics, and paleokarst environments. Karst reservoir characteristics were analyzed on the basis of the following analysis: (1) Karst morphological analyses based on core description and formation micro-imager (FMI) log analyses. The results showed that alveolar-like and Swiss cheese-like solution pores, spongy dissolution zones, pit cenotes, and small continuous karst caves developed in the Yingshan Formation. (2) The statistical analysis of pore and cave characteristics indicated that most of the karst pores and caves developed within 50 m below the unconformity where the average height of these features ranged from 0.1 to 3.0 m and their widths ranged up to 100 m. These pores and caves were commonly filled with gravel, clay, and calcite. Horizontal well and seismic attribute analysis indicated that these pores and caves were distributed over a large area. In plain view, the karst pore-cave system is comprised of cross-linked anastomosing networks of horizontal cave passages. And (3) Cathode luminescence and electron microprobe analyses suggested that clay filling within karst caves was freshwater related, while calcite filling was of seawater origin. Cements within solution pores showed three phases of luminescence, suggesting an alternating freshwater and seawater environment. Based on these characteristics, the karsts of the Yingshan Formation in the Tazhong area are interpreted to be similar to the eogenetic karsts in the Yucatan Peninsula of modern Mexico. Accordingly, this study indicates that the pore-caves of the Yingshan Formation can be subdivided into three sections. Further, the development and filling of these pore-cave sections are interpreted to have formed by eogenetic mixed-water karstification during three phases of relatively stable sea level in a coastal margin environment.

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van Beynen, Philip, Robert Brinkmann, and Kaya van Beynen. "A sustainability index for karst environments." Journal of Cave and Karst Studies 74, no. 2 (August 31, 2012): 221–34. http://dx.doi.org/10.4311/2011ss0217.

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Van Beynen, Philip, and Kaya Townsend. "A Disturbance Index for Karst Environments." Environmental Management 36, no. 1 (June 9, 2005): 101–16. http://dx.doi.org/10.1007/s00267-004-0265-9.

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Chen, Yue, Kangning Xiong, Xiaodong Ren, and Cai Cheng. "Vulnerability Comparison between Karst and Non-Karst Nature Reserves—With a Special Reference to Guizhou Province, China." Sustainability 13, no. 5 (February 24, 2021): 2442. http://dx.doi.org/10.3390/su13052442.

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Studying vulnerability has become one of the hot issues of ecological research under global change and sustainable development scenarios. However, there are few studies focusing on the vulnerability of karst areas, especially on the comparison between karst and non-karst areas. This study integrated climate factors, soil and vegetation factors, and social factors within a vulnerability evaluation framework that combined the analytical hierarchy process (AHP) technique to evaluate and compare the ecological environments of 10 karst nature reserves and five non-karst nature reserves in Guizhou Province, China. The evaluation results were divided into five categories: potential, light, moderate, severe, and extremely severe vulnerability. The results indicated that the general vulnerability of national nature reserves in Guizhou Province showed moderate vulnerability. The vulnerability index of karst nature reserves was significantly higher than that of non-karst nature reserves. The general vulnerability of karst nature reserves showed moderate vulnerability, while that of non-karst nature reserves showed light vulnerability. Average soil thickness, arable area, and the length of roads may be the factors contributing to the significant difference in the vulnerability between karst and non-karst nature reserves. Overall, this study is conducive to a comprehensive understanding of the ecological environment status of national nature reserves in Guizhou Province, and is of great significance to maintaining ecological security and sustainable development in karst areas.

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Sun, Shangqu, Liping Li, Jing Wang, Shuguang Song, Peng He, and Zhongdong Fang. "Reconstruction and Measurement of Irregular Karst Caves Using BLST along the Shield Metro Line." Applied Sciences 10, no. 1 (January 4, 2020): 392. http://dx.doi.org/10.3390/app10010392.

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This study investigated the application of the borehole laser scanning technology (BLST) method in the detection of both dry and water-filled karst caves. In order to solve the problem of excessive laser attenuation during the detection, we designed a test for the characteristics of multiwavelength laser attenuation in water-filled karst caves and studied the influence exerted by various factors, including different wavelengths, different laser power levels, different suspended media, and effect of turbidity on the attenuation coefficient. During the test, we discovered the existence of a “blue-green window” with low turbidity and a “near infrared window” with high turbidity in karst cave water environments. Based on the general survey results of drilling and comprehensive geophysical prospecting, a quantitative method using targeted drilling was proposed to detect the spatial morphology of karst caves in complex environments. We also investigated the effects of complex environmental factors such as suspended media and high turbidity on the laser detection distance and accuracy in karst caves, and established a quantitative matching model of laser wavelengths, laser power, and complex environmental parameters. Based on this, we obtained the best acquisition mode for detecting lasers in different karst development environments. A high-precision, three-dimensional visualized model of a real karst cave was established to quantitatively obtain the characteristic parameters, such as accurate position, three-dimensional shape, space volume, and cave filling type, which was applied to the detection of karst caves along the Jinan subway line.

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Conrado-Palafox, Alain L., Luisa N. Equihua-Anguiano, Marcos Orozco-Calderón, and Eleazar Arreygue-Rocha. "Numerical simulation of karst environments to study subsidence." Proceedings of the Institution of Civil Engineers - Geotechnical Engineering 172, no. 4 (August 2019): 365–76. http://dx.doi.org/10.1680/jgeen.18.00161.

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Epting, Jannis, Peter Huggenberger, and Lukas Glur. "Integrated investigations of karst phenomena in urban environments." Engineering Geology 109, no. 3-4 (November 2009): 273–89. http://dx.doi.org/10.1016/j.enggeo.2009.08.013.

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Palmer, A. N. "Deep-seated geochemical environments in karst: An introduction." Environmental Geology 25, no. 1 (February 1995): 1. http://dx.doi.org/10.1007/bf01061823.

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Dissertations / Theses on the topic "Karst Environments"

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Polk, Jason Samuel. "Proxy records of climate change in subtropical and tropical karst environments." [Tampa, Fla] : University of South Florida, 2009. http://purl.fcla.edu/usf/dc/et/SFE0003058.

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Sundqvist, Hanna S. "Speleothems as environmental recorders : A study of Holocene speleothems and their growth environments in Sweden." Doctoral thesis, Stockholm : Department of Physical Geography and Quaternary Geology, Stockholm University, 2007. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-1408.

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Justice, Brad L. "Modelling of Calcium Carbonate Precipitation in Natural Karst Environments Under Hydrodynamic and Chemical Kinetic Control." University of Akron / OhioLINK, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=akron1145310619.

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Tyrie, Elizabeth Katharyn. "Combining Quantitative Eye-Tracking and GIS Techniques with Qualitative Research Methods to Evaluate the Effectiveness of 2D and Static, 3D Karst Visualizations: Seeing Through the Complexities of Karst Environments." TopSCHOLAR®, 2014. http://digitalcommons.wku.edu/theses/1351.

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Karst environments are interconnected landscapes vulnerable to degradation. Many instances of anthropogenic karst disturbance are unintentional, and occur because of the public's lack of understanding or exposure to karst knowledge. When attempts are made to educate the general public about these landscapes, the concepts taught are often too abstract to be fully understood. Thus, karst educational pursuits must use only the most efficient and effective learning materials. A technique useful for assessing educational effectiveness of learning materials is eye-tracking, which allows scientists to quantitatively measure an individual's points of interest and eye movements when viewing a 2D or 3D visualization. Visualization developers use eye-tracking data to create graphics that hold the observer's attention and, thereby, enhance learning about a particular concept. This study aimed to assess and improve the educational effectiveness of 2D karst visualizations by combining eye-tracking techniques with Geographic Information Systems, knowledge assessments, and semi-structured interviews. The first phase of this study consisted of groups of 10 participants viewing 2D karst visualizations with one category of manipulated visual stimuli. The second phase consisted of groups of 10-15 participants viewing 2D karst visualizations that were created based on the results from the first phase. The results of this study highlighted both effective stimuli in karst visualizations and stimuli that hinder the educational effectiveness of visualizations.

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Jebreen, Hassan [Verfasser], Stefan [Gutachter] Wohnlich, and Frank [Gutachter] Wisotzky. "Karst water management in semi-arid environments: Central West Bank, Palestine / Hassan Jebreen ; Gutachter: Stefan Wohnlich, Frank Wisotzky ; Fakultät für Geowissenschaften." Bochum : Ruhr-Universität Bochum, 2019. http://d-nb.info/1182682316/34.

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Carlson, Justin Nels. "MIDDLE TO LATE HOLOCENE (7200-2900 CAL. BP) ARCHAEOLOGICAL SITE FORMATION PROCESSES AT CRUMPS SINK AND THE ORIGINS OF ANTHROPOGENIC ENVIRONMENTS IN CENTRAL KENTUCKY, USA." UKnowledge, 2019. https://uknowledge.uky.edu/anthro_etds/40.

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Though some researchers have argued that the Big Barrens grasslands of Kentucky were the product of anthropogenic land clearing practices by Native Americans, heretofore, this hypothesis had not been tested archaeologically. More work was needed to refine chronologies of fire activity in the region, determine the extent to which humans played a role in the process, and integrate these findings with the paleoenvironmental and archaeological record. With these goals in mind, I conducted archaeological and geoarchaeological investigations at Crumps Sink in the Sinkhole Plain of Kentucky. The archaeological record and site formation history of Crumps Sink were compared with environmental and archaeological data from the Interior Low Plateaus and Southern Appalachian Mountains for an understanding of how the site fits into the larger story of human-environmental interactions in the Eastern Woodlands. Based on the data recovered, I argue that through land burning Archaic hunter-gatherers were active managers of ecosystems to a greater degree than previously acknowledged. Excavations at Crumps Sink revealed stratified archaeological deposits spanning the late Middle Archaic to Terminal Late Archaic periods. Radiocarbon dates and an analysis of projectile point typologies provided information on the chronological and cultural history of the site. Magnetic susceptibility, loss-on-ignition, plant available phosphorous, and soil micromorphological analyses were conducted to examine landform dynamics in response to environmental change and to trace the anthropogenic signature created by human activities at the site. Masses of lithic debitage, animal bone, and burned sediment nodules per ten-cm-level provide an indication of human occupation intensity and shifting activities over time. Radiocarbon dates were used to reconstruct rates of sediment accumulation in the sink. These varying datasets were considered together for a holistic understanding of localized environmental and anthropogenic impacts on the landform. Between 7200 and 5600 cal. BP, during the Middle Holocene Thermal Maximum and corresponding with the late Middle Archaic period, sediment accumulation was sustained with one identifiable episode of very weak soil development. Background magnetic and chemical signatures in the soils were greater than they were at pre-occupation levels, demonstrating that human activities left a lasting imprint in soils as early as the late Middle Archaic period. Between 5600 and 3900 cal. BP, periods of diminished sedimentation led to more pronounced episodes of soil formation. However, these soil horizons are interposed by pulses of enhanced sediment accumulation. These soil data may signal shifting environmental regimes during the Middle to Late Holocene transition. Between 5600 and 3900 cal. BP scattered plant ash, elevated masses of burned sediment nodules, and pestle fragments in Late Archaic deposits suggest that hunter-gatherers were intensively processing nut mast, potentially in association with early forest clearance and silviculture. Botanical assemblages from a coincident archaeological sequence at the Carlston Annis site in the nearby middle Green River region has demonstrated woodland disturbance and potential silviculture in central Kentucky during this time. During the Late Archaic and Terminal Late Archaic periods (3900-3000 cal. BP), substantial plant ash deposition occurred in a stratum that accumulated relatively quickly. Very low burned sediment nodule masses in this deposit indicate that combustion features were not common in the immediate vicinity and that elevated frequencies of plant ash were the result of burning on a broader expanse of the surrounding landform. Chronologically, the zone with enhanced plant ash deposition is coeval with previously demonstrated occurrences of increased forest fires, grassland expansion, and a shift to early horticultural economies throughout the region. Soil development occurred after 3000 cal. BP, and this episode of landform stability may have lasted for over two millennia until being capped by sediment accumulation from historic agriculture. The late Middle Archaic through Terminal Late Archaic data from Crumps Sink demonstrate that hunter-gatherer activities left lasting signatures in soils in Kentucky. The data from the Late Archaic to Terminal Late Archaic periods (ca. 5600-3000 cal. BP) may indicate intentional land burning by hunter-gatherers to create anthropogenic environments, first for silviculture and then for early plant domestication. This forces a rethinking of labor and subsistence systems within hunter-gatherer societies. Thus, if hunter-gatherers were utilizing long-term forest management methods, they were employing a delayed-return economic system relying on labor investment and negotiated understandings about land tenure. Further characterization of the origin of fire management activities will help us to elucidate the nature of incipient indigenous plant domestication in the Eastern Woodlands.

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Hall, Veronica. "Addressing Water Resource Issues In Barbados Through An Isotopic and Atmospheric Characterization of Precipitation Variability." TopSCHOLAR®, 2014. http://digitalcommons.wku.edu/theses/1356.

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Numerous studies have analyzed isotopic variation of meteoric and dripwater in karst environments for paleoclimate reconstructions or aquifer recharge capacity. What is poorly understood is how the isotopic signal of δ18O and δ2H is transferred through the hydrologic cycle based upon storm type, frequency, intensity, and teleconnection activity in the tropical karst areas. At Harrison’s Cave, Barbados, a Hobo Onset event data logger was attached to a tipping bucket rain gauge to count the tips and record the total rainfall every 10 minutes. In the cave a Hobo data logger was used to record relative humidity and temperature at 10-minute intervals. Rainwater, dripwater, and stream water samples were collected at a weekly resolution and refrigerated before sample analysis. The study period was from July, 2012 to October, 2013, with data from the data loggers only until June, 2013 due to inability to reach the study site. The samples were analyzed using the Picarro Cavity Ring Down Spectroscopy Unit-Water L1102-I through laboratories at the University of Kentucky and the University of Utah. The samples were reported in per mil and calibrated. The teleconnection (NAO, AMO, and ENSO) and other atmospheric data were obtained from the Climate Prediction Center or the NOAA Earth System Research Laboratory-Physical Sciences Division. The weekly isotope signatures were linearly regressed against total rainfall for Harrison’s Cave and surface temperature with no statistically significant correlation, indicating the amount effect was not present at a weekly resolution. The amountweighted precipitation δ18O values were calculated on a monthly basis and compared to TRMM monthly rainfall and island-wide monthly rainfall, and a statistically significant negative correlation was found between both datasets. This confirmed that the amount effect dominates the island’s rainfall isotopic signature at a monthly resolution, and that specific atmospheric influences represented in weekly rainfall were less influential on a weekly basis. It is hypothesized that the variation in weekly rainfall is due to quick initiating, rain-out, and dissipation of convective storm systems over the island. In terms of evaporative influences, the samples do not deviate much from the Global Meteoric Water Line (GMWL), indicating minimal evaporation, which is typical for tropical locations. When the d-excess parameters were calculated, there were distinct variations with minimal evaporation occurring in the 2013 calendar year. This is attributed to coastal storm formation in the tropics.

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Schmidt, Sebastian [Verfasser], Martin [Akademischer Betreuer] Sauter, and Heinz [Akademischer Betreuer] Hötzl. "Hydrogeological characterisation of karst aquifers in semi-arid environments at the catchment scale – Example of the Western Lower Jordan Valley / Sebastian Schmidt. Gutachter: Martin Sauter ; Heinz Hötzl. Betreuer: Martin Sauter." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2014. http://d-nb.info/1059004526/34.

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Fleury, Spencer. "Land Use Policy and Practices in Karst Terrains." Scholar Commons, 2007. https://scholarcommons.usf.edu/etd/708.

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Karst topography is the result of a specific combination of geological conditions, precipitation, biota, and temperature, and is characterized by the gradual solution of the underlying bedrock and the development of underground drainage routes for surficial runoff. Many of these karst landscapes are found in urbanized areas, where the potential for anthropogenic impact is quite high. In many instances, municipalities on karst terrains choose to mitigate these impacts by implementing ordinances that place restrictions on permissible land uses near karst landforms. This dissertation asks the question: are the impacts of karst-related land use regulation on human / social systems significant enough to merit consideration during the regulation writing and implementation process? In the process of answering this question, it is hoped that a broader understanding will be developed of how land use regulations are used to control and regulate human activity on karst lands, particularly (but not exclusively) in the United States; and that the conclusions drawn from that overview might serve as the beginnings of a generally applicable framework for the development of karst regulation.

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Semler, Keith R. "Development of a Karst Tourism Management Index to Assess Tourism-Driven Degradation of Protected Karst Sites." TopSCHOLAR®, 2019. https://digitalcommons.wku.edu/theses/3143.

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The intent of this research was to create and evaluate a karst tourism management index (KTMI). This index is intended to be a new management tool designed to quantify environmental disturbances caused specifically by tourism activities in karst regions, particularly show caves and springs. In an effort to assess the effectiveness of the index as a management tool in karst terrains, after development, the index was applied to six case study sites. A review of the management policies at each study site was conducted with the use of standard policy critique methods and semistructured interviews with managers at the study sites. After interviews were completed, the newly created index was applied to the study areas with the aid of park land managers. Including land managers in the application process allowed for active land managers to provide more meaningful feedback on potential improvements to the KTMI to ensure the most universally applicable and thoroughly field-tested index tool was created. Upon application and continual refinement of the index to the six study sites, a new data-driven management tool to measure disturbances to karst terrains by tourism was developed. The KTMI consist of an Overall Score category that is broken down into the two main categories of Management and Tourism. The KTMI contains 168 indicators that all need to be scored individually to obtain results, with Management containing 100 of the indicators and Tourism containing the other 68 indicators.

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Books on the topic "Karst Environments"

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Veress, Márton. Karst Environments. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-3550-9.

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Veress, Márton. Karst environments: Karren formation in high mountains. Dordrecht: Springer, 2010.

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Multidisciplinary, Conference on Sinkholes and the Engineeering and Environmental Impacts of Karst (5th 1995 Gatlinburg Tenn ). Karst geohazards: Engineering and environmental problems in karst terrane : proceedings of the Fifth Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impact of Karst, Gatlinburg, Tennessee, 2-5 April 1995. Rotterdam, Netherlands: A.A. Balkema, 1995.

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International Speleological Congress (13th 2001 Brasília, Distrito Federal, Brazil). Speleo Brazil 2001: Speleology in the third millenium : sustainable development of karst environments : proceedings. Campinas, SP, Brazil: SBE, Sociedade Brasileira de Espeleologia, 2001.

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Younos, Tamim, Madeline Schreiber, and Katarina Kosič Ficco, eds. Karst Water Environment. Cham: Springer International Publishing, 2019. http://dx.doi.org/10.1007/978-3-319-77368-1.

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Karst in China: Its geomorphology and environment. Berlin: Springer, 1995.

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F, Beck Barry, Wilson William L, Feldman Laura, and Florida Sinkhole Research Institute, eds. Karst hydrogeology: Engineering and environmental applications : proceedings of the Second Multidisciplinary Conference on Sinkholes and the Environmental Impacts of Karst, Orlando/Florida/9-11 February 1987. Rotterdam: A.A. Balkema, 1987.

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Andreo, Bartolomé, Francisco Carrasco, Juan José Durán, Pablo Jiménez, and James W. LaMoreaux, eds. Hydrogeological and Environmental Investigations in Karst Systems. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-642-17435-3.

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Field, Malcolm S. A lexicon of cave and karst terminology with special reference to environmental karst hydrology. Washington, DC: National Center for Environmental Assessment--Washington Office, Office of Research and Development, U.S. Environmental Protection Agency, 2002.

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Field, Malcolm S. A lexicon of cave and karst terminology with special reference to environmental karst hydrology. Washington, DC: National Center for Environmental Assessment--Washington Division, Office of Research and Development, U.S. Environmental Protection Agency, 1999.

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Book chapters on the topic "Karst Environments"

1

Veress, Márton. "Introduction." In Karst Environments, 1–9. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_1.

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Veress, Márton. "Research Sites and Methods." In Karst Environments, 11–24. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_2.

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Veress, Márton. "Age and Characteristics of High Mountain Karren Formation." In Karst Environments, 25–35. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_3.

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Veress, Márton. "Karren Features." In Karst Environments, 37–152. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_4.

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Veress, Márton. "Karren Assemblages." In Karst Environments, 153–61. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_5.

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Veress, Márton. "Local Karren Belts." In Karst Environments, 163–77. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_6.

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Veress, Márton. "Coalescing of Karren Forms." In Karst Environments, 179–213. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-90-481-3550-9_7.

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van Beynen, Philip E., and Kaya M. van Beynen. "Human Disturbance of Karst Environments." In Karst Management, 379–97. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1207-2_17.

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Humphreys, William F. "Management of Groundwater Species in Karst Environments." In Karst Management, 283–318. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-94-007-1207-2_13.

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Dreybrodt, Wolfgang. "Precipitation of Calcite in Natural Environments." In Processes in Karst Systems, 256–72. Berlin, Heidelberg: Springer Berlin Heidelberg, 1988. http://dx.doi.org/10.1007/978-3-642-83352-6_10.

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Conference papers on the topic "Karst Environments"

1

Albright, Lydia, and Greg Springer. "HYDRAULIC MODELING OF FLOODS IN OPEN CONDUIT KARST ENVIRONMENTS." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-337957.

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Druhan, Jennifer L., Jessica L. Oster, and Corey Lawrence. "A REACTIVE TRANSPORT DESCRIPTION OF CARBON TRANSPORT AND TRANSFORMATION IN KARST ENVIRONMENTS." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-285306.

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Yue, Yuemin, Kelin Wang, Bo Liu, and Ru Li. "Estimation of fractional vegetation cover based on spatial continuity within heterogeneous karst environments." In 2012 Second International Workshop on Earth Observation and Remote Sensing Applications (EORSA). IEEE, 2012. http://dx.doi.org/10.1109/eorsa.2012.6261190.

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Noury, Gildas, Jérôme Perrin, Li-Hua Luu, Pierre Philippe, and Sébastien Gourdier. "Role of Floods on Sinkhole Occurrence in Covered Karst Terrains: Case Study of the Orléans Area (France) During the 2016 Meteorological Event and Perspectives for other Karst Environments." In National Cave and Karst Research Institute Symposium 7. National Cave and Karst Research Institute, 2018. http://dx.doi.org/10.5038/9780991000982.1014.

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Scabbia, Giovanni, and Essam Heggy. "Assessing Sub-Wavelength VHF Radar Scattering Losses in Dry Terrains: Application to Karst Environments." In IGARSS 2019 - 2019 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2019. http://dx.doi.org/10.1109/igarss.2019.8899032.

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Richardson, Jr., Jesse J. "Judge Dillon and Karst: Limitations on Local Regulation of Karst Hazards." In 10th Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. Reston, VA: American Society of Civil Engineers, 2005. http://dx.doi.org/10.1061/40796(177)56.

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Islam, M. Zia, and Aravinda M. Ramakrishna. "Highway Widening in Karst." In 10th Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. Reston, VA: American Society of Civil Engineers, 2005. http://dx.doi.org/10.1061/40796(177)37.

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Black, Tyrone J. "Evaporite Karst in Michigan." In Ninth Multidisciplinary Conference on Sinkholes and the Engineering and Environmental Impacts of Karst. Reston, VA: American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40698(2003)12.

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Ross, D. Lauren. "Product Pipeline Hazards over Karst Aquifers." In National Conference on Environmental and Pipeline Engineering. Reston, VA: American Society of Civil Engineers, 2000. http://dx.doi.org/10.1061/40507(282)57.

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Wang, Chengliang, Mingzhou Bai, and Chengyong Yang. "Study on Monitoring and Warning System of Karst Water Bursting Disaster in Karst Area." In 2016 5th International Conference on Sustainable Energy and Environment Engineering (ICSEEE 2016). Paris, France: Atlantis Press, 2016. http://dx.doi.org/10.2991/icseee-16.2016.36.

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