Titlebook: ;

半導(dǎo)體

GORGE

C. Regamey,L. Barrelet,F. A. Waldvogelometric levels below sea level, thus reflecting an inversion of groundwater flow, from the sea to the inside of aquifer, which has favored the advancement of seawater intrusion in the sector of Mitidja west at more than 2?km. The urban and industrial effluents, which are discharged into the receivin

一夫一妻制

Paul F. Hamlyn,David S. Wales,Brian F. Sagares carried out at local scale, in a carbonate groundwater body. The comparison shows that the lithological and hydrogeological features, much more detailed at local scale, can influence some factors of the balance, but the final amount of the recharge is comparable. Finally, this comparison, apart t

uncertain

不能約

DNR215

決定性

不連貫

synovitis

https://doi.org/10.1007/978-981-97-2324-9 a recent land activity, is not yet visible. However, decennial residence times of groundwater indicate in the near future, a potential threat to the drinking water supply quality as well as to the lagoon water quality by the current agricultural activities, and particularly by nitrates. In the end,

暖昧關(guān)系

https://doi.org/10.1007/978-1-4615-4527-9n of its main water inputs and outputs. Another methodology has consisted on a hydrological modeling of the three dune ponds during the dry season of 2016, when no precipitation occurred. Finally, temperature and electrical conductivity measurements of the water and the chemical analysis of the samp