نتایج جستجو برای: deep seawater

تعداد نتایج: 223348  

Journal: :Sustainable Cities and Society 2021

In tropical climates, the energy consumed by heating, ventilation and air conditioning can exceed 50% of total consumption a building. The demand for cooling is rising steadily, driven global warming rapidly increasing living standards in developing economies. addition, there rise water due to population increase, life quality, warming. Coastal areas with narrow continental shelves are perfect ...

Journal: :Journal of the Chinese Medical Association : JCMA 2013
Chin-Wen Chi

Fatty liver disease is a growing health concern in western and other developed countries. The cause of fatty liver can be broken down into two categories: (1) alcoholic fatty liver disease and (2) nonalcoholic fatty liver disease (NAFLD). The abnormal retention of fat as vacuole in hepatocytes is more commonly known as steatosis and can progress further to steatohepatitis, possibly resulting in...

Journal: :Journal of the Chinese Medical Association 2013

2001
Michael H. Huesemann

In an attempt to reduce the threat of global warming, it has been proposed that the rise of atmospheric carbon dioxide concentrations be reduced by the ocean disposal of CO2 from the flue gases of fossil fuel-fired power plants. The release of large amounts of CO2 into mid or deep ocean waters will result in large plumes of acidified seawater with pH values ranging from 6 to 8. In an effort to ...

Journal: :Analytical sciences : the international journal of the Japan Society for Analytical Chemistry 2011
Keiichi Fujimori Kenta Tsujimoto Takayo Moriuchi-Kawakami Yasuhiko Shibutani Masato Ueda Takahiko Suzue Hideshi Kimoto Kei Okamura

A new chemiluminescence method is proposed for the determination of sulfide in seawater based on the chemiluminescence reaction between sulfide and an acidic permanganate solution. 3-Cyclohexylaminopropanesulfonic acid was used as a chemiluminescence enhancer. By use of this method, 1-150 µM of sulfide could be determined in artificial seawater. The limit of detection was 0.17 µM sulfide. We in...

2010
J. W. de Baar Cindy Lee

Novel methods were developed for the determination of 12 of the 14 Rare Earth Elements (REE) in seawater. Initial extractions of the REE by chelating ion exchange chromatography is followed by cation exchange for removal of co-extracted U and remaining traces of major ions. Finally traces of U are removed by anion exchange before irradiation for 8 hours at a flux of 5 x 1013 neutrons.cm-2 .sec~...

Journal: :Applied and environmental microbiology 2008
Tara L Harmer Randi D Rotjan Andrea D Nussbaumer Monika Bright Andrew W Ng Eric G DeChaine Colleen M Cavanaugh

Recent evidence suggests that deep-sea vestimentiferan tube worms acquire their endosymbiotic bacteria from the environment each generation; thus, free-living symbionts should exist. Here, free-living tube worm symbiont phylotypes were detected in vent seawater and in biofilms at multiple deep-sea vent habitats by PCR amplification, DNA sequence analysis, and fluorescence in situ hybridization....

2017
Clément P Bataille Amy Willis Xiao Yang Xiao-Ming Liu

The composition of igneous rocks in the continental crust has changed throughout Earth's history. However, the impact of these compositional variations on chemical weathering, and by extension on seawater and atmosphere evolution, is largely unknown. We use the strontium isotope ratio in seawater [(87Sr/86Sr)seawater] as a proxy for chemical weathering, and we test the sensitivity of (87Sr/86Sr...

1999
Thomas Pichler Jan Veizer

Ž . Previous research on sea floor Fe III oxyhydroxide deposits has focused primarily on deep-sea, hydrothermal systems found along volcanically active portions of the mid-ocean ridges and on hydrogenetic deposits formed in deep basins and along continental shelves. There is, however, not much known about their formation in shallow-water settings associated with volcanic islands. The hydrotherm...

2012
J. A. Higgins D. P. Schrag

Deep-sea pore fluids are potential archives of ancient seawater chemistry. However, the primary signal recorded in pore fluids is often overprinted by diagenetic processes. Recent studies have suggested that depth profiles of Mg concentration in deep-sea carbonate pore fluids are best explained by a rapid rise in seawater Mg over the last 10–20 Myr. To explore this possibility we measured the M...

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