[Durcansky et. al., Vol.7 (Iss.5): May 2019] ISSN- 2350-0530(O), ISSN- 2394-3629(P) DOI: https://doi.org/10.29121/granthaalayah.v7.i5.2019.846 Http://www.granthaalayah.com ©International Journal of Research - GRANTHAALAYAH [278] Science PRIMARY ENERGY ACCUMULATION THROUGH ADVANCED GAS HYDRATES SYSTEM Peter Durcansky *1 , David Hecko 1 , Milan Malcho 1 1 University of Žilina, Faculty of Mechanical Engineering, Department of Power Engineering, Univerzitna 1, 010 26 Žilina, Slovakia Abstract Accumulation of primary energy of natural gas is a perspective industrial area mainly for countries dependent on the import of energy and raw materials. Transporting and storage of natural gas is economically and technologically demanding, which is always reflected in the resulting price. Natural gas hydrates allow transport and storage at low pressures and relatively favorable temperatures. Another no less important area is the storage of energy in biogas plants where gas formation is time-dependent. Biogas hydrates would allow short-term storage at room temperature and atmospheric pressure. This article deals with the design of a functional prototype for the production of hydrates and numerical simulation. Keywords: Primary; Energy; Accumulation; Hydrates System. Cite This Article: Peter Durcansky, David Hecko, and Milan Malcho. (2019). “PRIMARY ENERGY ACCUMULATION THROUGH ADVANCED GAS HYDRATES SYSTEM.” International Journal of Research - Granthaalayah, 7(5), 278-283. https://doi.org/10.29121/granthaalayah.v7.i5.2019.846. 1. Introduction Gas Hydrate as Energy Storage The storage of natural gas in hydrates is particularly advantageous in terms of storage capacity, but also in terms of gas storage safety, which is possible at higher temperatures and lower pressures compared to other storage technologies such as liquefaction or compression. The gas hydrate can be a great source of energy that begins to be included in the considerations of gas supply for the next decades. It is estimated that 99% of the global gas hydrate supply occurs in marine sediments under the corresponding temperature and pressure conditions, in seabed sediments, at depths from 300 m to 4000 m. [1, 2]