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

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31#
發(fā)表于 2025-3-26 22:33:17 | 只看該作者
32#
發(fā)表于 2025-3-27 01:47:28 | 只看該作者
David B. Herbstxt? that covers the wide range of evidences on the NAO impacts in the Mediterranean regions and from a multidisciplinary perspective. .?This volume constitutes a unique document to present the state of the art 978-94-007-3648-1978-94-007-1372-7Series ISSN 1574-0919 Series E-ISSN 2215-1621
33#
發(fā)表于 2025-3-27 05:56:33 | 只看該作者
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發(fā)表于 2025-3-27 21:26:21 | 只看該作者
37#
發(fā)表于 2025-3-27 23:54:27 | 只看該作者
,Hydrogeochemistry of Lake Gallocanta (Aragón, NE Spain),m). In addition to these fluctuations, seasonal changes of the water level between 20 and 50 cm occurred every year..Gallocanta is a Na-Mg-Cl-(SO.) type lake. During the drying period a typical salt enrichment occurs with linear relationships between TDS, Cl, Na and K. Alkalinity is linearly correla
38#
發(fā)表于 2025-3-28 06:10:21 | 只看該作者
Vernal microstratification patterns in a meromictic saline lake: their causes and biological signifnto two layers above the primary chemocline. The several year persistence of the secondary chemoclines and associated interface processes (concentration of particulate organic matter, bacterial decomposition, nutrient regeneration, phytoplanktonic production) attest to their functional importance in
39#
發(fā)表于 2025-3-28 08:50:19 | 只看該作者
Production and decomposition processes in a saline meromictic lake,in a dense layer (POC 250 mg1., bacteriochlorophyll . 1500–7000 μg1.), where H.S changed from 0.1 to 2.5 mM over a 0.2 m depth interval. This phototrophic bacterial layer contributed between 17.66% of the total primary production (115–476 mgC m. d.) in the vertical water column. Microorganisms in th
40#
發(fā)表于 2025-3-28 11:55:59 | 只看該作者
Autumnal mixing in Mahoney Lake, British Columbia,n efficiency factor of 0.20 for the penetrative convection energy, larger than values previously reported in the literature, was found to fit the measured loss of potential energy of stratification during the period.
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