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本文简要地介绍了我们开创的流变学的一个新分支学科——流变断裂学的主要成果。应用这一新理论,我们成功地解释了拓溪水电站单支墩大头坝迎水面上垂直裂纹的发生与发展。
This article briefly introduces a new subdiscipline of rheology that we pioneered, the main result of rheological fractures. Applying this new theory, we successfully explained the occurrence and development of vertical cracks on the flood surface of a single-headed pier with a large span at the Tuoxi Hydropower Station.