Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱渗、耦合行为是影响土类工程岩体的稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱渗、耦合行为是影响土类工程岩体的稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体的强度和稳定性的重。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体的强度和稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体强度和稳定性重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50风吹雨打后，恶地国家公园黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体的强度和稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历50年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体的强度和稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱、应力耦合行为是影响土类工程岩体的强度性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一片草原之海中。

Coupled unsaturated flow in claystone has high effect on strength and stability of underground engineering.

非饱和渗流、应力耦合行为是影响土类工程岩体的强度和稳定性的重要因素。

Whittled by a half million years of wind and rain, the haunting claystone hills and buttes of Badlands National Park rise above the surrounding sea of grasslands.

历经了50万年的风吹雨打后，恶地国家公园的黏土岩丘陵与孤山矗立在一之海中。