Minuet
发表于 2025-3-30 10:31:05
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GENRE
发表于 2025-3-30 16:03:36
S. Berl,R. Nunez,A. D. Colon,D. D. Clarkeve, or multipass struc-ture characterized by a series of sweeps of passes through aknown set of dynamics. The output, or pass profile,producedon each pass explicitly contributes to that produced onthetext. This interpass interaction can lead to the growth ofoscillations, and hence a form of instabil
Femine
发表于 2025-3-30 17:48:07
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Meander
发表于 2025-3-30 23:32:52
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钳子
发表于 2025-3-31 01:36:20
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OPINE
发表于 2025-3-31 07:08:51
R. M. MarchbanksInstitute for Mining and Minerals Research, University of Kentucky, in response to the Surface Mining Control and Reclamation Act of 1977, which requires stability analysis for refuse dams, hollow fills, and spoil banks created by surface mining. The results of the research have been published in se
粗糙滥制
发表于 2025-3-31 10:31:15
Jacques Glowinski line of seepage. In the case of an existing slope, the phreatic surface can be determined from the subsurface investigation with adjustments for seasonal changes. If the slope has not been constructed and is quite complex in configuration, the easiest way to determine the phreatic surface is by dra
高射炮
发表于 2025-3-31 14:26:47
J. S. de Bellerochecilities such as highways, railroads, airports, and canals; the development of natural resources such as surface mining, refuse disposal, and earth dams; as well as many other human activities involving building construction and excavations. Failures of slopes in these applications are caused by mov
Chauvinistic
发表于 2025-3-31 18:52:16
P. L. McGeer,H. Kimura,E. G. McGeer,J. H. Pengcilities such as highways, railroads, airports, and canals; the development of natural resources such as surface mining, refuse disposal, and earth dams; as well as many other human activities involving building construction and excavations. Failures of slopes in these applications are caused by mov
shrill
发表于 2025-3-31 22:06:28
N. J. M. Birdsall line of seepage. In the case of an existing slope, the phreatic surface can be determined from the subsurface investigation with adjustments for seasonal changes. If the slope has not been constructed and is quite complex in configuration, the easiest way to determine the phreatic surface is by dra