DEAWL 发表于 2025-3-28 17:01:50

Dagmar Schmelzerensors, infrared and other sensors. The modern researches of UAVs with a manipulator are discussed, including those devoted to the problems of flight control, avoidance of contact with the ground, interaction with the surrounding space, as well as physical interaction with ground-based objects. The

泥瓦匠 发表于 2025-3-28 21:33:57

Ralf Junkerjürgenrofiles. One of those native houses had been burned, and was readily interpreted using the magnetic maps superimposed on the GPR maps. It appears that from the geophysical mapping and some excavations that native people and colonists from England lived in close proximity to each other, but preferred

PATHY 发表于 2025-3-29 02:02:08

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钳子 发表于 2025-3-29 03:17:14

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欢乐东方 发表于 2025-3-29 10:58:23

Patrick Eseristemologie und Methodologie eher plausibel anhört, erweist sich in der praktischen Forschungsarbeit als kaum brauchbar. Hier ist es meist wichtig, zu strikte oder zu simple Polarisierungen zu vermeiden. Martyn Hammersley (1992, S.80: vgl. auch Hülst 2010, S.283) hat zurecht darauf hingewiesen, dass

cutlery 发表于 2025-3-29 14:23:25

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AMEND 发表于 2025-3-29 15:36:33

Claudia Jünkeause of the way they conceived the ontological status of accidents. Against the second objection, I show that while Henry admits the possibility of self-agency as a consequence of his view of the nature of causal powers, Scotus thinks that without self-agency one cannot account for why proper and in

occurrence 发表于 2025-3-29 22:22:25

Claudia Jünkeotropy of permeability (../.. = 10) and the radius (4 to 16 metres) of the horizontal conductive fractures crossed by the wells. Two different scales of fracture networks are identified: the primary fracture network (PFN), which affects the matrix on a decimeter scale by contributing to an increase

Cryptic 发表于 2025-3-30 01:04:46

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Obloquy 发表于 2025-3-30 05:05:40

Sabine Friedrichg of .; (ii) Estimation of one variable based on measurements of other variables: co-estimation of piezometric head and transmissivity; (iii) Estimation of the gradient of . at an arbitrary site: estimation of groundwater flow velocity based on observed heads; (iv) Estimation of the integral of . ov
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