Titlebook: Saline Lakes; Proceedings of the F Franciso A. Comín,Thoma G. Northcote Conference proceedings 1990 Kluwer Academic Publishers 1990 Fauna.b

Intimidate

書目名稱Saline Lakes影響因子(影響力)




書目名稱Saline Lakes影響因子(影響力)學科排名




書目名稱Saline Lakes網絡公開度




書目名稱Saline Lakes網絡公開度學科排名




書目名稱Saline Lakes被引頻次




書目名稱Saline Lakes被引頻次學科排名




書目名稱Saline Lakes年度引用




書目名稱Saline Lakes年度引用學科排名




書目名稱Saline Lakes讀者反饋




書目名稱Saline Lakes讀者反饋學科排名

歡呼

Nutrients in pore waters from Dead Sea sediments,ilization, reduction of sulfate and formation of iron sulfides and accumulation of ammonia. Mass balance calculations show that pore water contribute about 80% of the ammonia and 30% of the phosphate input into the Dead Sea water column. On the other hand, the sediments act as a sink for carbonate and sulfate.

含糊

Diluge

Sediment-water interaction as a control on geochemical evolution of playa lake systems in the Austrse lakes mark the outcrop areas of regional shallow groundwater; thus, they are effective hydro-chemical sinks for elemental concentration and authigenic formation of carbonate, evaporite, and silica/silicate minerals..Field observations and petrochemical characterization of playa sediments from dra

LIKEN

instill

Cleave

The evolution of saline lake waters: gradual and rapid biogeochemical pathways in the Basotu Lake D East Africa). Examination of 11 (out of 13) lakes in the Basotu Lake District identified two distinct evolutionary pathways: a gradual path and a rapid path. During the course of biogeochemical evolution these waters follow either the gradual path alone or a combination of the gradual and rapid pat

刺激

小卒

DECRY