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。

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50万年雨打后，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。

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.

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.

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。

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。