• Aucun résultat trouvé

Saturated groundwater flow (Chapter 4 - Hydrogeology course)

N/A
N/A
Protected

Academic year: 2021

Partager "Saturated groundwater flow (Chapter 4 - Hydrogeology course)"

Copied!
2
0
0

Texte intégral

Loading

Références

Documents relatifs

Second, in zone 3, at Les Rubattiers-Leschaux (left bank, KP111 to KP110), the three methods diverged over a small distance: the macrophyte index did not highlight groundwater

In Central Asia, the Amu Darya River Basin (ADRB) which namely covers part of Afghanistan and the former soviet republics of Tajikistan, Uzbekistan and Turkmenistan,

It is shown here that in the case of coupling groundwater flow and hydrological models – in particular on the regional scale – it is very impor- tant to find a common definition

In particular, we show that (1) the inability to simulate negative pressures beneath disconnected streams in MODFLOW results in an underestimation of the infiltration flux; (2) a

This scheme is qualitatively consistent with the 0%, 33% and 16% of water coming from the aquifer calculated with the groundwater flow model for the same

The key faultlines at the COP focused on the level of emissions commitments for industrialised and advanced developing countries, verifi cation of emissions reductions and policies,

This block detects the start frame of the protocol and determines the number of following UART frames attached to this message.. It then treats the received data to determine if

Karstic processes evolution in the Risle river, their impacts on surface water/groundwater interaction, river flow loss dynamics study and impacts on groundwater... Karstic