热力作用是与应力、重力相类同的一类地质作用力。
Thermal action is a kind of geological force similar to stress and gravity.
此外，还发现有早期(石炭纪—二叠纪)岩浆热力作用事件。
Besides, we also find that there are magma thermal actions during the Carboniferous period and early Permian period.
最后对大跨屋面结构在非对称热力作用下的极限状态进行了分析。
Further study on large - span dome structure is carried out to investigate its limit - state behavior due to non-symmetric heating.
各个热力作用面的热力特征和相互作用将制约林窗的热力变化，影响植物的生长。
The thermal variations of canopy gap of forest are controlled by the thermal characteristics of different thermal active surfaces and by their interaction, affecting the growth of plants.
否则有机物质就会遭热力作用而转化成毫无价值的非碳氢化合物——黑色含炭物质。
Or the organic material will be transformed by heat into a non-hydrocarbon black carbonaceous material of no value.
热带季节雨林中热力作用复杂、多样，使得热力效应时空分布趋于多样化，导致小气候环境异质性。
Thermal effect of tropical seasonal rain forest is so complicated and multiform that makes thermal effect distribution diversification and induces microclimatic environment heterogeneity.
建立了青藏高原热力作用和气候变化的关系及其对青海湖水位下降趋缓(年际差增大)的概念模型。
So a concept model has been get up by above research, this model explain that how the thermal in the Qinghai-Xizang Plateau effects on the water level in Qinghai Lake through basin climate change.
三是不同尺度地形条件的动力作用，和沙漠与戈壁下垫面的热力影响。
Third, the dynamics action of different scale topography, and the heating power influence on desert and Gobi under layer.
利用弹塑性介质的不可逆热力学的普遍关系，对弹粘塑性孔隙介质在冲击静水压力作用下的力学行为进行了研究。
The mechanical behaviors of elastoviscoplastic porous media subjected to hydrostatic shock are studied here in the framework of irreversible thermodynamics of elastoviscoplastic media.
在登陆台风减弱过程的不同阶段，热力和动力作用很不相同。
In the various weakening stages of the landed typhoon, the thermodynamic and dynamic processes were different.
在登陆台风减弱过程的不同阶段，热力和动力作用很不相同。
In the various weakening stages of the landed typhoon, the thermodynamic and dynamic processes were different.
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