Debris flow泥石流地质英语论文.doc
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1、地质英语结课论文学 号 03210337 姓 名 班 级 10级地质三班Debris flowDebris flow is between flow and landslide between a geological processes.The typical debris flow by suspended the bulky solid debris and rich in silt and clay sticky mud composition. In the appropriate terrain conditions, a large number of water penetra
2、tion hillside or ditch the solid bed accumulation of material, make its stability is reduced, full of water accumulation of solid material in its own gravity happened under movement, they form a debris flow. Debris flow is a severe geological phenomenon. Debris flow often suddenly broke out, feral,
3、can carry huge stones, and with high speed, with a strong energy, thus can be very destructive. It broke out suddenly, feral, of great destructive power.The whole process of debris flow generally only a few hours, short only a few minutes. Debris flow is a widely distributed all over the world some
4、with special topography, physiognomy status areas of natural disasters. Is the mountain valleys or mountain slope surface, by the heavy rain, ice and snow melting water and stimulate, contains a lot of sediment rocks between carrying water flow and landslide between the soil, water, gas mixed flow.
5、Most of the debris flow with mountain flood and happen. It and general flood is the difference between stream contains a sufficient number of sediment stone, solid debris, the volume content at least 15%, the highest can amount to 80% or so, so more destructive than the flood.Debris flow influence t
6、he intensity of many factors, such as debris flow capacity, velocity and flow rate and so on, the debris flow discharge of debris flow hazard degree of impact on the most main. In addition, a variety of human activities in many aspects and intensifying the above factors effect, promote the formation
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