Engineering Geology World Vol. XIV, No. 1/2019
OLEG B. NESHCHETKIN, MAKSIM O. NESHCHETKIN
Neshchetkin O.B, Neshchetkin M.O., 2019. Sinkhole development model. Part 2. Investigation of the structure of sinkholes in nature. Engineering Geology World, Vol. XIV, No. 1, pp. 44-58, https://doi.org/10.25296/1993-5056-2019-14-1-44-58.
The main methods of sinkhole research in nature were: the morphometric method, excavations of sinkholes, cone penetration test (CPT) and drilling in the sinkhole zones, the study of the kinematic and dynamic characteristics of the sinkholes and accompanying effects. The study of morphological features of the sinkhole parameters has allowed to establish, that almost everywhere the appearance of the sinkholes corresponds to the elementary geometric shapes: arched — cylindrical — conical — cupped — saucer-shaped. In the case where the covering deposits are represented by clayey soils, most of the karst sinkholes have an arched or cylindrical shape and conical and cupped forms are typical for sandy soils. Excavations of karst sinkholes have established the arch character of the collapse of soils in the intermediate cavity in the development of a sinkhole on the earth’s surface. The CPT of the sinkhole zones revealed specific features of the soil decompaction in the sinkhole, which testify to the collapse of the soils into the intermediate cavity. Drilling operations in the conditions of carbonate and sulphate karst have established that the intermediate cavities develop over the karst cavities. In 2015, the authors were lucky to observe the sequence of the sinkhole development on the earth’s surface and to distinguish three stages of the sinkhole formation. The results of karst sinkholes investigations in nature conditions and laboratory modeling of the mechanism of their formation are in good agreement and clearly indicate that the destruction of the cover soils over the karst cavities in the collapse of their roofs begins with the formation of a primary intermediate cavity the surface of which is described by an arch of natural equilibrium. Further, there is a successive collapse of the arch of this primary intermediate cavity and the formation of an intermediate cavity at a lower depth. Thus, the intermediate cavity “moves” to the earth’s surface. In the initial stage of formation of a sinkhole on the earth’s surface, concentric cracks appear and a small saucer-shaped lowering, the formation of an arch sinkhole occurs in the main stage, in the final stage there is a collapse and displacement of blocks of soil with formation of a depression of a steady state.
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OLEG B. NESHCHETKIN*
Scientific Production Center KARST LLC; Dzerzhinsk, Nizhny Novgorod Region, Russia; karst@sinn.ru
Address: Bld. 3, Butlerova St., 606000, Dzerzhinsk, Nizhny Novgorod Region, Russia
MAKSIM O. NESHCHETKIN
Scientific Production Center KARST LLC; Dzerzhinsk, Nizhny Novgorod Region, Russia; karst@sinn.ru