Project Geothermal Mongolia Description

Description

Introduction

The existence of numerous hot springs in Mongolia’s Hangai province is indicative for large geothermal energy resources, which are remnants of the region’s volcanic geological history. Previous studies have shown that a combined, geothermal heat and power plant could provide cheap and clean energy for the province center Tsetserleg. With this project we will introduce the missing geophysical component of the so far conducted geothermal exploration program in the Hangai. We will establish scientific methods to image the geothermal reservoir near Tsetserleg, which feeds the hot springs in Tsenkher and Shivert. The result will be of great importance for promoting the construction of geothermal power plant.

This project is a collaboration between ETH Zurich and the Mongolian Academy of Sciences. It is funded by the Swiss Programme for Research on Global Issues for Development (r4d programme) – a joint funding initiative by the Swiss Agency for Development and Cooperation (SDC) and the Swiss National Science Foundation (SNSF).

Objectives

Hot rock in the subsurface, a remnant from
Hangai’s volcanic history, heats fluids in the underground. Some of the fluids migrate upwards along permeable geological faults, where they result in hot springs as observed in Tsenkher. This hot spring has a flow rate of more than 10l/s and a temperature that exceeds 80°C.
With this project we will conduct magnetotelluric (MT) measurements during two field campaigns in 2019 and 2020. Based on the MT data it is possible to construct a 3-D geothermal reservoir model in order to evaluate the potential for heating and energy production. We will use our new MT geophysical soundings for a consistent interpretation together with previously conducted geochemical and geological studies.
Conceptual ModelConceptual model for the geothermal system near Tsetserleg and proposed power plants.

Geographic scope

The measurements will be taken in the hot spring area south of Tsetserleg during field surveys in May-June 2019 and 2020. In the first survey we plan to measure on an array with 2km site spacing. In the second survey we will refine our measurement array around the Tsenkher hot springs and around an 450m deep exploration well near Tsetserleg.

Relevance

The capacity of a geothermal CHP plant in Tsetserleg could reach 1.9 MWe power and 16.7 MWt heat production as shown in a study by Purevsurem Dorj from the National Renewable Energy Center in Ulaanbaatar (Dorj, 2005 and 2015). Such a plant would even exceed the current power and heat consumption in Tsetserleg. Geothermal energy could be a great benefit to all inhabitants. It would result in massively reduced greenhouse gas emissions and lead to improved live and working conditions.

Fieldwork Impressions

References

Comeau, M. J., Käufl, J. S., Becken, M., Kuvshinov, A., Grayver, A. V., Kamm, J., … & Batmagnai, E. (2018). Evidence for fluid and melt generation in response to an asthenospheric upwelling beneath the Hangai Dome, Mongolia. Earth and Planetary Science Letters, 487, 201-209.
Dorj, P. (2005), Thermoeconomic analysis of a new geothermal utilization CHP plant in Tsetserleg, Mongolia, Master’s thesis, The United Nations University.
Dorj, P. (2015), Geothermal development in Mongolia: Country update, in Proceedings of the World Geothermal Congress, Melbourne, Australia.
Ganbat, E., and O. Demberel (2010), Geologic background of the Hangay geothermal system, West-Central
Mongolia, in Proceedings World Geothermal Congress, Bali, Indonesia.
Oyuntsetseg, D., Ganchimeg, D., Minjigmaa, A., Ueda, A., & Kusakabe, M. (2015). Isotopic and chemical studies of hot and cold springs in western part of Khangai Mountain region, Mongolia, for geothermal exploration. Geothermics, 53, 488-497.