Titlebook: Dynamics and Geomorphology of Mountain Rivers; Peter Ergenzinger,Karl-Heinz Schmidt Book 1994 Springer-Verlag Berlin Heidelberg 1994 Fests

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書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers影響因子(影響力)




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers影響因子(影響力)學(xué)科排名




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers網(wǎng)絡(luò)公開(kāi)度




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers網(wǎng)絡(luò)公開(kāi)度學(xué)科排名




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers被引頻次




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers被引頻次學(xué)科排名




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers年度引用




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書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers讀者反饋




書(shū)目名稱(chēng)Dynamics and Geomorphology of Mountain Rivers讀者反饋學(xué)科排名

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LUCY

Anthropoid

River channel adjustment and sediment budget in response to a catastrophic flood event (Lainbach ca than eroded, resulting in an overall mass balance surplus of about 35000 m.. A large part of this material was mobilized in the tributary channels and slope rills. Slope failures were only of minor importance, characterizing this catastrophic event as a channel flood. The flood caused a fundamental

placebo-effect

Condense

Condense

Short term temporal variations in bedload transport rates: Squaw Creek, Montana, USA and Nahal Yatibasis of trap filling rates. The temporal nature of sediment transport in both environments is similiar, as indicated by repeated pulsing. Short term bedload fluctuations are independant of the discharge magnitude but dependant on its duration or change in magnitude.

KIN

Measuring systems to determine the velocity field in and close to the roughness sublayer,ng systems were tested. The received data show system dependent relationships. Thus, it is important to consider errors and failures that can be related to the utilized LDA-system. A description of the three different LDA-systems as well as a list of errors and failures and a short summary of main r

Substance-Abuse

An attempt at determination of incipient bed load motion in mountain streams,07–0.14 m. The standard deviation of the grain size distribution was variable δ=1.8–3.2..The presented investigations concern the floods, when the maximum water flow was Q.=5.50 m./s, Q.=2.75 m./s, Q.=5.75 m./s, Q.=5.90 m./s. The amounts of the transported bed material during these floods were: G.=6

FEMUR

Q.W.L. developments in Holland: an overview snow in many different ways, e.g. to generate hydroelectric power, for irrigation and, especially during the winter, for recreation purposes. Soil compaction on ski-runs leads to a very high velocity of discharge, which results in an increasing rate of erosion in these areas..Furthermore, factors s