Search citation statements
Paper Sections
Citation Types
Year Published
Publication Types
Relationship
Authors
Journals
Works on the construction of the foundation pit for the dam of the Kurpsa hydroelectric station began following the completion of the temporary diversion tunnel and damming the Naryn River [i].After the rock was excavated in the side cuts for the dam, excavation began in the channel part of the pit, where in an extremely short time (1.5-2 months) it was required to excavate about 60,000 m 3 of earth. The dimensions of the dam pit are: width ii0 m and length 90 m. Immediately adjacent to it is the ll0gm wide, ll5-m-long foundation pit for the powerhouse.Upper Carboniferous flysch deposits, represented by interstratified sanastones of strength group VIII with respect to the Construction Norms and Regulations (SNIP) (up to 75%) and argillites of group VII (up to 25%) occur in the base of the pits. The rock surface in the channel is uneven. There were a largenumber of grooves and individual depressions filled with fluvial deposits with various particles sizes. The thickness of the alluvial deposits reached 5 m.The foundation rocks were broken by various tectonic joint systems and bedding joints. With respect to the degree of fracturing the rocks belong to the II category (severely fractured, medium-block) according to the provisional classification [2]. The rocks in the channel are severely waterlogged. There was flowing water (recharge from the upper pool) in the rock mass over the entire section being excavated. The plan of the pits is shown in Fig. i. The contract design called for loosening the near-contour layer by 105-mm-diameter borehole charges with a 1.5 m-thick protective layer being left. The protective layer was to be finished in two levels: the upper 1-m-thick level with loosening by means of blasthole charges with manual pneumatic drilling and the lower 0.5-m-thick level by means of picks.However, it was impossible to accomplish the design scheme, since even in stretches of the river where the rock outcropped the blastholes and even the 105-mm-diameter boreholes, drilled by rigs with a submersible compressed-air drill (NKR-100M), after extracting the drilling tool either collapsed or were very quickly filled with sand and cuttings owing to the strong inflow of water. An intense technology of excavation with loosening of the rocks by charges of 130-mm-diameter sticks of explosives in holes bored by BTS-150 rigs was developed.To protect the base of the pit from destruction the holes were drilled short so that the boundary of the explosive disturbance of the natural state of the mass did not exceed the limits of the design outlines of the pit.The size of the zone of disturbance was determined by the method developed at the AllUnion Trust for Special Hydraulic Engineering Works (Gidrospetsproekt) [311 The calculated depth of the zone of penetration of blast deformations into the mass was 12 charge diameters. In conformity with this, the bottom of the charges was 1.5 m from the base. To determine more accurately the effect of the explosion into the mass, experimental clearing to the undamaged rock was perfor...
Works on the construction of the foundation pit for the dam of the Kurpsa hydroelectric station began following the completion of the temporary diversion tunnel and damming the Naryn River [i].After the rock was excavated in the side cuts for the dam, excavation began in the channel part of the pit, where in an extremely short time (1.5-2 months) it was required to excavate about 60,000 m 3 of earth. The dimensions of the dam pit are: width ii0 m and length 90 m. Immediately adjacent to it is the ll0gm wide, ll5-m-long foundation pit for the powerhouse.Upper Carboniferous flysch deposits, represented by interstratified sanastones of strength group VIII with respect to the Construction Norms and Regulations (SNIP) (up to 75%) and argillites of group VII (up to 25%) occur in the base of the pits. The rock surface in the channel is uneven. There were a largenumber of grooves and individual depressions filled with fluvial deposits with various particles sizes. The thickness of the alluvial deposits reached 5 m.The foundation rocks were broken by various tectonic joint systems and bedding joints. With respect to the degree of fracturing the rocks belong to the II category (severely fractured, medium-block) according to the provisional classification [2]. The rocks in the channel are severely waterlogged. There was flowing water (recharge from the upper pool) in the rock mass over the entire section being excavated. The plan of the pits is shown in Fig. i. The contract design called for loosening the near-contour layer by 105-mm-diameter borehole charges with a 1.5 m-thick protective layer being left. The protective layer was to be finished in two levels: the upper 1-m-thick level with loosening by means of blasthole charges with manual pneumatic drilling and the lower 0.5-m-thick level by means of picks.However, it was impossible to accomplish the design scheme, since even in stretches of the river where the rock outcropped the blastholes and even the 105-mm-diameter boreholes, drilled by rigs with a submersible compressed-air drill (NKR-100M), after extracting the drilling tool either collapsed or were very quickly filled with sand and cuttings owing to the strong inflow of water. An intense technology of excavation with loosening of the rocks by charges of 130-mm-diameter sticks of explosives in holes bored by BTS-150 rigs was developed.To protect the base of the pit from destruction the holes were drilled short so that the boundary of the explosive disturbance of the natural state of the mass did not exceed the limits of the design outlines of the pit.The size of the zone of disturbance was determined by the method developed at the AllUnion Trust for Special Hydraulic Engineering Works (Gidrospetsproekt) [311 The calculated depth of the zone of penetration of blast deformations into the mass was 12 charge diameters. In conformity with this, the bottom of the charges was 1.5 m from the base. To determine more accurately the effect of the explosion into the mass, experimental clearing to the undamaged rock was perfor...
The development of water-power construction in the USSR can be divided into several periods: the first --realization of the plan proposed by the State Commission for the Electrification of Russia; the second --the prewar period, which saw the exploitation of the Dnepr and Volga rivers and the Caucasian and Kola peninsulas, and the initial explltatlon of the rivers of Central Asia; the third --the post-war period, which saw the rapid completion of the exploitation of the Volga and Dnepr and Trans-Caucasla and the start of construction on hydroelectric plants in Siberia; the fourth --the systematic exploitation of the Angara and Enisei and the start of construction on the first hlgh-head hydraulic facilities; the modern period --the construction of hlgh-head hydro projects in the alpine and foothill regions of Siberia, the Far East, Central Asia, Northern Caucasia, and Trans-Caucasia.In the initial period, water power was based on fundamental studies of prominent Russian scientists of the prerevolutlonary period, and on foreign experience and techniques in practical matters. Later, the development of water-power construction in the USSR took a course that differred markedly from foreign experience. This was determined by the need for the rapid solution of the most complex problems on which the developed capitalist countries had a considerable head start and by the natural construction conditions, which differred from those in the European countries. All this served to create the Soviet school of water-power construction, which had captured substantial international authority. The services rendered by the journal G~otekhn~cheskoe Stz, oitel'stvo, which since its establishment, has taken a leading position in shedin8 light on problems associated with water-power construction, and, particularly, in problems involving the organization and production of work, have been important to the creation of the school. Since the first years, the Journal has been an aid to Soviet, and, recently, to foreign specialists.The journal has exposed and promulgated basic ideas concerning the improvement of such trends in water-power construction as: the overall organization of construction; the closure of river channels and the organization of the concrete, rock-crushing, gravel-screenlng and other establishments required for the building of hydraulic structures; the mechanization of concrete and earthwork, and mechanism for the production of these operations; the compositions of concrete mixes; study of the thermal-stressed state of dams; tunneling, dewaterlng, and consolidation operations; and, the assembly of metallic hydraulic designs and hydraulic equipment and other trends in the organization and production of work.
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.
customersupport@researchsolutions.com
10624 S. Eastern Ave., Ste. A-614
Henderson, NV 89052, USA
This site is protected by reCAPTCHA and the Google Privacy Policy and Terms of Service apply.
Copyright © 2024 scite LLC. All rights reserved.
Made with 💙 for researchers
Part of the Research Solutions Family.