483 14TH SINKHOLE CONFERENCE NCKRI SYMPOSIUM 5 LEPT, A SIMPLIFIED APPROACH FOR ASSESSING KARST VULNERABILITY IN REGIONS BY SPARSE DATA: A CASE IN KERMANSHAH PROVINCE, IRAN Kamal Taheri Groundwater and Karst expert in Kermanshah Regional Water Authority, Kermanshah, Iran, Taheri.kamal@gmail.com Milad Taheri Bu-Ali Sina University, Hamadan, Iran, milad.thr@gmail.com Fathollah Mohsenipour Head of groundwater study group in Kermanshah Regional Water Authority, Kermanshah, Iran data base; therefore, there is a need for a method that could be applied with the least amount of available data. The LEPT method introduced in this paper is a simple approach which provides rough evaluation of the general information gathered from karst areas of the west of Iran combined with field experiments. This method, which utilizes four parameters to assess the vulnerability of karst aquifers, was applied to the karst areas of Kermanshah (a province in the west of Iran) for the first time. Results of this approach categorize karst plains into four zones with very high, high, low and very low sensitivity in terms of their vulnerability to environmental impact. These classes are positively correlated with field information. Introduction Despite its undeniable role in drinking water supply for both rural and urban areas, karst aquifers are highly vulnerable to contamination. In some cases, presence of thin or no soil cover, shallow depth/thickness of karst aquifer overburden (epikarst zones) and direct point recharge via swallow holes make these water resources more susceptible to contamination by a variety of anthropogenic pollutants. On the other hand, because of the high groundwater velocity, short residence time of pollutants in karst aquifers affects the processes of contaminant attenuation in karst systems (Goldscheider, 2005). This is especially true in bare or thinly covered karst terrains. Comprehension of the level of sensitivity of karst aquifers to contamination and provision of a thorough karst management strategy can establish an effective framework for planning and scheduling protection programs. Several researchers have shown keen interest in groundwater protection since Margat (1968) and Albinet Abstract There are a variety of widely used methods for porous aquifer protection to assess the vulnerability of groundwater resources, such as DRASTIC; Depth to water, net Recharge, Aquifer media, Soil media, Topography, Impact of vadose zone, and hydraulic Conductivity, SINTACS; depth to ground water (S), effective infiltration (I), unsaturated zone attenuation capacity (N), soil attenuation capacity (T), hydrogeologic aquifer characteristics (A), hydraulic conductivity range (C) and hydrological role of the topographic slope (S). And GOD; Groundwater occurrence, Overlying lithology, and Depth of groundwater. However, some more limited methods (including EPIK; Epikarst development, Protective cover, Infiltration conditions and Karst network development, PaPRIKa; Protection of karst Aquifers based on their Protection, Reservoir, Infiltration and Karstification type and COP; Concentration of flow, Overlying layers, and Precipitation regime) are also suggested for karstic aquifer vulnerability analysis. The latter methods are applied using different parameters such as karst network development, depth of karstification, and protective cover. Due to the nature of the data, these methods are highly affected by local and regional climate conditions. Data gathering for these methods is difficult, time consuming and needs a full understanding of karst systems. Data shortages, especially those related to karst formations in some parts of the world including the west part of Iran, and crucial demands for utilizing water resources demonstrate a great appeal to find a representative method for evaluation of these regions. Conventional methods of karst aquifer evaluation cannot be properly applied in the absence of a required karst