REGIONAL FEATURE OF LEOSS-LIKE SUBSIDENCE CLAYEY SOILS COMMON IN MONGOLIA

Authors

  • S.Nyamdorj Institute of Sivil Engeenring Mongolian National Technical University, Ulaanbaatar
  • D.Dashjamts Construction and Architectural Institute Mongolian State University of Science and Technology,Ulaanbaatar
  • Kh.Bayanmunkh Institute of Sivil Engeenring Mongolian National Technical University, Ulaanbaatar

Keywords:

initial settling pressure, initial settling moisture, soaking, relative settling, pile foundations, artificial foundations

Abstract

In connection with the regional climatic and geographical features of Mongolia, loose soil deposits of the Quaternary period of the Cenozoic era are common at the depth of the foundations of buildings and below, such as loess-like subsidence and swelling clay soils, permafrost soils, heaving soils during seasonal freezing, eluval, etc. From this, the innovative application of optimal experimental and theoretical solutions for foundations and the preparation of artificial foundations, taking into account regional characteristics, is an important scientific and national economic task.

Published

2022-10-06

How to Cite

S.Nyamdorj, D.Dashjamts, & Kh.Bayanmunkh. (2022). REGIONAL FEATURE OF LEOSS-LIKE SUBSIDENCE CLAYEY SOILS COMMON IN MONGOLIA. Theoretical Hypotheses and Empirical Results, (1). Retrieved from https://ojs.publisher.agency/index.php/THIR/article/view/15

Issue

No. 1 (2022): Theoretical Hypotheses and Empirical Results

Section

Geological and mineralogical sciences