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Hydrogeological Atlas of Rajasthan Baran District

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Hydrogeological Atlas of Rajasthan Baran District Baran District Hydrogeological Atlas of Rajasthan Baran District Contents: List of Plates Title Page No. Plate I Administrative Map 2 Plate II Topography 4 Plate III Rainfall Distribution 4 Plate IV Geological Map 6 Plate V Geomorphological Map 6 Plate VI Aquifer Map 8 Plate VII Stage of Ground Water Development (Block wise) 2011 8 Location of Exploratory and Ground Water Monitoring Plate VIII 10 Stations Depth to Water Level Plate IX 10 (Pre-Monsoon 2010) Water Table Elevation Plate X 12 (Pre-Monsoon 2010) Water Level Fluctuation Plate XI 12 (Pre-Post Monsoon 2010) Electrical Conductivity Distribution Plate XII 14 (Average Pre-Monsoon 2005-09) Chloride Distribution Plate XIII 14 (Average Pre-Monsoon 2005-09) Fluoride Distribution Plate XIV 16 (Average Pre-Monsoon 2005-09) Nitrate Distribution Plate XV 16 (Average Pre-Monsoon 2005-09) Plate XVI Depth to Bedrock 18 Plate XVII Map of Unconfined Aquifer 18 Glossary of terms 19 2013 ADMINISTRATIVE SETUP DISTRICT – BARAN Location: Baran district is located in the southeastern part of Rajasthan. It is bounded in the east by state of Madhya Pradesh, southwest by Jhalawar district and northwest by Kota district. It stretches between 24⁰ 23' 35.85” to 25⁰ 26' 39.94” North latitude and 76⁰ 11' 34.16’’ to 77⁰ 25' 56.74’’ East longitude covering area of 6,994 sq kms. Major part of the district has a systematic drainage system, as whole district is part of ‘Chambal River Basin’. Administrative Set-up: Baran district is administratively divided into seven Blocks. The following table summarizes the basic statistics of the district at block level. Population Area % of District Total Number of S. No. Block Name (Based on 2001 census) (sq km) Area Towns and Villages 1 Antah 1,97,385 1,033.3 14.8 158 2 Atru 1,32,944 946.4 13.5 139 3 Baran 1,81,807 638.8 9.1 103 4 Chhabra 1,22,268 798.9 11.4 193 5 Chhipabarod 1,43,885 684.3 9.8 181 6 Kishanganj 1,35,218 1,450.4 20.7 203 7 Shahbad 1,08,146 1,441.9 20.7 236 Total 10,21,653 6,994.0 100.0 1,213 Baran district has 1,213 towns and villages, of which seven are block headquarters as well. Climate: The district has a sub-humid climate, moderately dry and receives fairly good rainfall in monsoon seasons. The winter season extends from November to February and summer season from March to mid of June. The period from mid of June to September is the monsoon season followed by the months October to mid of November constitutes the post monsoon or the retreating monsoon. The mean annual rainfall in the district is 838.7mm. January is the coldest month with the average daily maximum temperature of 24.3 ⁰C and the average daily minimum temperature in the range of 8-10 ⁰C. 1 2 TOPOGRAPHY DISTRICT – BARAN The topography of Baran district is in general, undulating in in the western part, but hilly in the eastern and southern parts constituting predominant landforms visible in Shahbad, Chhabra and Chhipabarod blocks. The general topographic elevation in the district is between 250 m to 450 m above mean sea level. The narrow elongated hills rise up to 548.8 m elevation in eastern part of the district. Apart from the well-known Chambal River, the other rivers that flow through the districts are Andheri and Kali Sindh and their tributaries are Bambidai, Kui, Kosam, Khari, Bllas and Samranla. Elevation ranges from a minimum of 200 m above mean sea level in Antah block in the northwestern part of the district to a maximum of 548.8 m above mean sea level In Shahbad block in eastern part of the district. Table: Block wise minimum and maximum elevation Minimum Elevation Maximum Elevation S. No. Block Name (m amsl) (m amsl) 1 Antah 200.0 288.3 2 Atru 252.2 429.5 3 Baran 207.7 293.5 4 Chhabra 281.0 488.9 5 Chhipabarod 290.5 471.5 6 Kishanganj 212.2 442.9 7 Shahbad 283.9 548.8 RAINFALL The rainfall is very scanty and erratic. The general distribution of rainfall across can be visualized from isohyets presented in the Plate – III where most of the district received rainfall in the range of 600-700 mm in year 2010. The annual average rainfall was 621.2 mm based on the data of available blocks. Maximum Annual rainfall was noticed in Atru block (724.4 mm) whereas minimum was in Antah block (562.0 mm). The highest average annual rainfall noticed in Chhipabarod block. Table: Block wise annual rainfall statistics (derived from year 2010 meteorological station data) Minimum Annual Maximum Annual Average Annual Block Name Rainfall (mm) Rainfall (mm) Rainfall (mm) Antah 445.2 697.8 614.9 Atru 584.6 724.4 667.9 Baran 512.8 639.8 599.5 Chhabra 557.1 685.8 590.6 Chhipabarod 616.3 705.5 675.2 Kishanganj 578.0 669.1 616.0 Shahbad 568.3 612.0 584.0 3 4 GEOLOGY DISTRICT – BARAN Most of the part of Baran district is occupied by rocks of Vindhyan Super Group. On the basis of different rock-units the Vindhyans of the area have been divided in to Bhander, Rewa and Khorip Groups comprising Shale, Limestone and Sandstones. The Khorip Group is separated from Rewa Group by conglomerate horizon. The Southern part of Chhabra and Chhipabarod block is occupied by Deccan trap basalt. Bhander Group occupies most part of the district. Super Group Group Formation Recent Alluvium (Sand, Silt, Clay) Deccan trap Basalt --X--------X--------X--------X---Unconformity---X--------X--------X-------X-- Bhander Shale, Limestone, Sandstone Vindhyan Rewa Shale --X--------X--------X--------X---Unconformity---X--------X--------X-------X-- Lower Vindhyan Khorip Shale, Limestone, Sandstone GEOMORPHOLOGY Table: Geomorphologic units, their description and distribution Origin Landform Unit Description Buried Pediment Pediment covers essentially with relatively thicker alluvial, colluvial or weathered materials. Denudational Broad gently sloping rock flooring, erosional surface of low relief between hill and plain, comprised of varied lithology, Pediment criss-crossed by fractures and faults. Mainly undulating landscape formed due to fluvial activity, comprising of gravels, sand, silt and clay. Terrain mainly Alluvial Plain undulating, produced by extensive deposition of alluvium. Fluvial Formed by fluvial activity, usually at lower topographic locations, comprising of boulders, cobbles, pebbles, gravels, Valley Fill sand, silt and clay. The unit has consolidated sediment deposits. Ravine Small, narrow, deep, depression, smaller than gorges, larger than gulley, usually carved by running water. Structural Dissected Plateau Plateau, criss-crossed by fractures forming deep valleys. Steep sided, relict hills undergone denudation, comprising of varying lithology with joints, fractures and lineaments. Denudational, Structural Hills Linear to arcuate hills showing definite trend-lines with varying lithology associated with folding, faulting etc. Hill, Linear Ridge Long narrow low-lying ridge usually barren, having high run off may form over varying lithology with controlled strike. 5 6 AQUIFERS DISTRICT – BARAN Aquifers in Baran district are formed in Sandstone, Limestone, Basalt, Shale and Younger alluvium. Weathered and fractured parts of the massive rocks along with primary and secondary openings in Sandstones and Limestone respectively, contribute to aquifer formation whereas the sandy, gravelly and other granular parts of alluvium constitute aquifers. Vindhyan sandstones are the most prevalent aquifer types with more than 52% spatial coverage and present prominently in the central part of the district. The Basalt aquifers occupy about 16% of the district area and present in southern part of the district. Shales and Limestones constitute aquifers in the eastern and western parts of the district respectively. Alluvium constitutes small patch of sandy aquifers around Baran contributing to less than 5% of aquifer area to the district. Table: aquifer potential zones their area and their description Aquifer in Potential Area % age of Description of the unit/Occurrence Zone (sq km) district It is largely constituted of Aeolian and Fluvial sand, silt, clay, gravel and Younger Alluvium 327.1 4.7 pebbles in varying proportions. In general, it is fine to medium grained, grey, red yellowish, pink or buff Limestone 1204.3 17.2 in colour. Sandstone 3670.0 52.5 Fine to medium grained, red colour and compact and at places. Shale 622.8 8.9 Grey, light green and purple in colour and mostly splintery in nature. Dark grey, olive green and green colour, compact, vesicular, Basalt 1,141.7 16.3 amygdaloidal and weathered. Hills 28.1 0.4 Total 6,994.0 100.0 STAGE OF GROUND WATER DEVELOPMENT The different blocks of the district fall into three categories of ground water development stages. Shahbad, the easternmost block falls into ‘safe’ category whereas further west the Kishangarh block is under ‘semi-critical’ category. The rest of the blocks constituting a strip along the western part of the district, fall under over-exploited category indicating the areas where steps need to be taken to reduce stress on ground water due to exploitation. Categorization on the basis of stage of Block Name development of ground water Safe Shahbad Semi- Critical Kishanganj Over Exploited Antah, Baran, Atru, Chhipabarod, Chhabra. Basis for categorization: Ground water development <= 70% - Safe; >70%; >90% - Semi critical and >100% - Over-Exploited. 7 8 LOCATION OF EXPLORATORY AND GROUND WATER MONITORING WELLS DISTRICT – BARAN The district has a well distributed network of large number of exploratory wells (47) and ground water monitoring stations (170) in the district owned by RGWD (43 and 154 respectively) and CGWB (4 and 16 respectively). The exploratory wells have formed the basis for delineation of subsurface aquifer distribution scenario in three dimensions.
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