The Discovery of Helium Gas in South Ganga Basin, Sagar Division M P India

Recent Advances in Petrochemical Science ISSN: 2575-8578

Arun K Shandilya*, Anurag Shandilya and Anupam Shandilya Department of Applied Geology, Dr HSG University, India Submission: October 10, 2019; Published: November 06, 2019 *Corresponding author: Arun K Shandilya, Department of Applied Geology, Dr HSG University, Sagar MP, India

Keywords: Petroleum gas; Tube wells; Hydrocarbon; Geochemical; Isotopic analyses; Soil; Water; Gas samples; Methane; Ethane; Oxygen; Nitrogen; Carbon dioxide; Sandstone; Sodium chloride solution; Glass bottles; Butane; Reservoir; Biogenic and thermogenic gas

Opinion condition. These gases were formed in the later phase of folding A rare Discovery of the Helium and Petroleum Gas in more in the Lower, Middle and Upper Vidhyan rocks. In the gently than 54 Tube wells in and around Sagar Town in Sagar Division folded rocks around Sagar area also containing these gases. The (1993 to 2015 period) in the rocks of Upper Rewa sandstone of the Vindhyan Super group. The discovery of the Rare Gas Helium the values for the methane is - 43.6 per mil w. r. t. to - 54.9 per stable Isotopic analysis suggests the stable isotope δ C13 value mil w.r.t. PDB and for the Ethane gas is --24.9 to --26.4 per mil in hydrocarbon rich zone in the tube wells in agricultural field in w. r. t. PDB in the gas samples collected in the saturated sodium of the Vindhyan Super Group, in the history of Earth Science the Villages in Sagar division of M P is a unique finding in rocks chloride solution in the glass bottles at various sites in Sagar & in India. The depth of tube wells is varying in 300 feet to 1000 Damoh District. feet. On the basis of Geochemical & Stable Isotopic analyses of the soil, water and gas samples held at Geochemical Lab of The occurrence of rare helium gas in the Hydrocarbon rich KDM IPE, ONGC, Dehradun and National Geophysical Research Institute (NGRI) Hyderabad, it is remarkable to note that average Sagar Distt, which were geochemically and stable isotopically zone is reported first time in Jan 2007 from the tube wells of values of rare gas helium contents varies from 0.34 % to 0.732 % analyzed in the labs of KDMIPE Dehradun & NGRI Hyderabad. The along with the 72% to 99 % of methane and ethane, and minor gaseous hydrocarbon analysis shows the presence of moderate amount of oxygen, nitrogen and CO2 gases in the hydrocarbon to low concentration of methane (C1) 1 to 104 ppb, Ethane(C2)-1 rich zone are recorded. In the west central part of the Vindhyan to 14 ppb, Propane(C3) 1 to 10 ppb, i- Butane (i C4) 1 to 9 ppb Basin around sagar area is characterized by the presence of the and n Butane (nC4) 1 to 8 ppb in the soil samples collected from Helium along with hydrocarbon gas in Upper Sandstone rocks of different locations. The Isotopic composition of the hydrocarbon Rewa group, which was overlain by the Deccan trap Basaltic lava gases are governed by their source of characteristic. In case of the thermogenic gases the maturity of the parent kerogen at sandstone. the time of gas generation also affect the isotopic composition flow, iot6 is acting as trap or cover rocks over theses gaseous of the gas. The migration does not appear to affect the isotopic The occurrence of the various inlier of the Vindhyan rocks are signature of the hydrocarbon gases, although due to diffusion contain the Helium and hydrocarbon gases. In variably we do not through imperfect seals in a reservoir, isotopically lighter 12C get the gas during the mansoon period, after the mansson period, methane may preferentially escape leaving behind isotopically after Nov. every year there is leakages of both the gases coming behavior gas in a reservoir. Biogenic and Thermogenic gas can from the tube wells. The part of the Vindhyan basin, which is not be distinguished based on molecular and isotopic composition. covered with the Deccan trap basalt, do not have any chances of storing these gases/rare gases. During the intrusion of the Dome The Biogenic gases are depleted in higher hydrocarbon gas, structure of Jabera area in Damoh Distt, about 140km east of like ethane, propane, butane etc. The methane is biogenic gas if the study are, must be responsible for the generation of these gases by the fractionation under high temperature & pressure Sandstone of Rewa group of of rocks of the Vindhyan Super Group the isotopic value of the δ C13 -55%. The helium gas in the Upper

Recent Adv Petrochem Sci 7(1): RAPSCI.MS.ID.555701 (2019) 001 Recent Advances in Petrochemical Science are generated from thermal cracking of U238 (U238- Pb206 + per mill w.r.t. PDB are indicative that this gas is of thermogenic He) and Kerogen. No mixing with any biogenic gas taken place origin, which must have been formed at very high temperature & after the generation of thermogenic gases. The Result of the soil pressure condition in the deeper horizon of the Great Vindhyan gas and stable isotopic analysis of Ethane gas in these samples sedimentary basin of late Proterozoic (> 600 m.y.) period.

δ C13value are ranging from -24.9 per mill w.r.t. PDB and -26.9 This work is licensed under Creative Your next submission with Juniper Publishers Commons Attribution 4.0 License DOI: 10.19080 RAPSCI.2019.07.555701 will reach you the below assets • Quality Editorial service • Swift Peer Review • Reprints availability • E-prints Service • Manuscript Podcast for convenient understanding • Global attainment for your research • Manuscript accessibility in different formats ( Pdf, E-pub, Full Text, Audio) • Unceasing customer service

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How to cite this article: Nief Rahman Ahmed. Promethazine an Environmental Friendly Reagent for Novel Spectrophotometric Method Estimation of Hypochlorite 002 in Different Environmental Samples. Recent Adv Petrochem Sci. 2018; 6(5): 555700. DOI: 10.19080 RAPSCI.2018.06.555700