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Earth dams REASONS FOR permafrost

机译:土坝永久冻土的原因

摘要

1. Ground Based dam on permafrost comprising upstream and downstream of the prism, the nucleus, the upstream and downstream transition layers, veil thermal placed along the dam in the zone of transition layers grassroots and formed as a series of contiguous wells, each of which is equipped with at least one heating device, and arranged on the downstream side of the core at the bottom of the dam drainage catchment part is arranged in positive temperature zone, characterized in that it is provided with means ohm to create a center pole cores positive temperatures and water taking part drainage at the bottom of the downstream prism at the bottom of the river bed and has direct access to the river, the water taking drainage portion is riprap high whose permeability when operating fluctuations in the downstream layers water in a river constantly provides a drainage portion in the plenum of positive temperatures due to the periodic input - output heating river water into the pores of riprap vodootvo dyaschey portion drainage by increasing - decreasing the water level in reke.2. Dirt dam according to claim 1, characterized in that in the case of inclusion of the dam in the lower part of a retaining wall made of concrete and the waterproof directly adjacent to the core by the tailrace comprising in its body gallery and providing a pass over the building itself spring flood, gallery is provided with a retaining wall heating device providing picture heating cavity and drainage catchment part is placed in the positive ones zone
机译:1.多年冻土上的地基坝,包括棱镜的上游和下游,原子核,上游和下游的过渡层,沿坝位于过渡层基层区域的面层热,并形成一系列连续的井,每个井设有至少一个加热装置,并布置在大坝排水集水部分底部的芯子的下游侧,布置在正温度区,其特征在于,它设有欧姆以产生正极中心的芯子温度和取水量在河床底部的下游棱柱底部排泄并直接通向河道,取水排泄部分的跳动性很高,当下游层中的水不断波动时其渗透性不断由于周期性的输入而在通风系统的正压力中提供排水部分-输出加热的河水进入riprap的孔中通过增加-减少reke中的水位来排出vodootvo dyaschey部分。2。 2.根据权利要求1所述的污物坝,其特征在于,在将所述坝包括在由混凝土制成的挡土墙的下部中的情况下,并且通过在其主体通道中包括的尾部赛道直接与所述核心相邻的防水层建筑物本身是春季洪水,画廊设有挡墙加热装置,提供图像加热腔,排水集水部分位于正面区域

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