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Fig 1.

Mining subsidence damages and ground fissures in Wanli Town, Dongsheng District, Erdos City, Inner Mongolia, China.

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Fig 1 Expand

Fig 2.

Directions of layer movements caused by subsidence in a flat coal seam.

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Fig 2 Expand

Fig 3.

Results of conventional physical similar simulation tests.

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Fig 3 Expand

Table 1.

Geological conditions in model (ratio of similitude 100:1).

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Table 1 Expand

Fig 4.

The accomplished two-dimensional plane model.

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Fig 4 Expand

Table 2.

Similar material properties.

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Table 2 Expand

Fig 5.

The hydraulic loading devices.

(A) “RSC–1050” jacks and “CP–180” hydraulic pump. (B) Spring-steel plate mechanisms.

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Fig 5 Expand

Table 3.

“RSC–1050” jacks’ parameters.

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Table 3 Expand

Fig 6.

The final model of Test 1.

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Fig 6 Expand

Fig 7.

Quasi-three-dimensional high-pressure hydraulic loading simulation experiment platform.

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Fig 7 Expand

Fig 8.

The simulation hydraulic support with working resistance monitoring sensor.

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Fig 8 Expand

Table 4.

Geological conditions in model (ratio of similitude 100:1).

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Table 4 Expand

Table 5.

Similar material properties.

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Table 5 Expand

Fig 9.

The physical model of Test 2.

(A) Mixture of materials. (B) Compaction of materials. (C) Mica powder for layer separation. (D) The accomplished model.

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Fig 9 Expand

Fig 10.

Two cases with and without three-hinged arch structure.

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Fig 10 Expand

Fig 11.

Slots set on the right side of the models.

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Fig 11 Expand

Fig 12.

Overlying strata movement and breakage during the excavation.

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Fig 12 Expand

Fig 13.

Overlying strata movement and breakage during the excavation.

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Fig 13 Expand

Table 6.

The distance of fracture ahead, initiation angle and fracture angle at different position.

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Table 6 Expand

Fig 14.

Overlying strata movement and breakage before excavated to 70cm.

Note: “60b”means the coal wall is at 60cm but the support is at 50cm and doesn’t lower, “60a”means the coal wall is at 60cm and the support lowers at 50cm.

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Fig 14 Expand

Fig 15.

Overlying strata movement and breakage when excavated to 70–100cm.

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Fig 15 Expand

Fig 16.

Overlying strata movement and breakage when excavated to 130cm and 180cm.

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Fig 16 Expand

Fig 17.

Overlying strata movement and breakage when excavated to 180cm.

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Fig 17 Expand

Fig 18.

Overlying strata movement and breakage after finished excavation.

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Fig 18 Expand

Table 7.

The distance of fracture ahead, initiation angle and fracture angle at different position.

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Table 7 Expand

Fig 19.

The stress of the hydraulic support during the caving process.

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Fig 19 Expand

Fig 20.

Mechanical model of roof’s fracture.

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Fig 20 Expand

Fig 21.

The three-hinged arch structure.

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Fig 21 Expand

Fig 22.

Stress distribution in beam.

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Fig 23.

Stress distribution in beam under different l.

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Fig 23 Expand

Fig 24.

Crack initiation angle under different shift step distance.

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Fig 24 Expand

Fig 25.

The breakage when excavated to 100cm.

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Fig 25 Expand

Fig 26.

Stress distribution in beam under different l.

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Fig 26 Expand