Terminal lakes

Terg-O-Tometer Terg-o-tometer Terlinguaite [12394-37-5] Termamyl Terminal lakes Terminal sterilization Ternary polymer blends Terne metal... 

Minerals of sodium sulfate occur naturally throughout the world. The deposits result from evaporation of inland seas and terminal lakes. Colder climates, such as those found ia Canada and the former Soviet Union, favor formation of mirabilite. Warmer climates, such as those found ia South America, India, Mexico, and the western United States, favor formation of thenardite. In areas where other anions and cations are present, double salts can be found of the kiads shown ia Table 2, which Hsts nearly all naturally occurring minerals containing sodium sulfate. Except for mirabilite, thenardite, and astrakanite, these mineral deposits play a minor role ia sodium sulfate production. 

A second source of brine is found in terminal lakes. The Dead Sea in Israel and Jordan is an example of a large terminal lake with almost unlimited supphes of magnesium chloride, potassium chloride, and sodium chloride. Mote than two and a half million tons of potassium chloride ate extracted from the Dead Sea each year. 

Great Salt Lake, Utah, is the largest terminal lake in the United States. From its brine, salt, elemental magnesium, magnesium chloride, sodium sulfate, and potassium sulfate ate produced. Other well-known terminal lakes ate Qinghai Lake in China, Tu2 Golu in Turkey, the Caspian Sea and Atal skoje in the states of the former Soviet Union, and Urmia in Iran. There ate thousands of small terminal lakes spread across most countries of the world. Most of these lakes contain sodium chloride, but many contain ions of magnesium, calcium, potassium, boron, lithium, sulfates, carbonates, and nitrates. 

A third source of brine is found underground. Underground brines ate primarily the result of ancient terminal lakes that have dried up and left brine entrained in their salt beds. These deposits may be completely underground or start at the surface. Some of these beds ate hundreds of meters thick. The salt bed at the Salat de Atacama in Chile is over 300 m thick. Its bed is impregnated with brine that is being pumped to solar ponds and serves as feedstock to produce lithium chloride, potassium chloride, and magnesium chloride. Seades Lake in California is a similar ancient terminal lake. Brine from its deposit is processed to recover soda ash, borax, sodium sulfate, potassium chloride, and potassium sulfate. 

Occurrence. About half of all the sodium chloride [7647-14-5J produced in the wodd is from brine. Approximately one hundred million tons pet year are produced from brines of the ocean, terminal lakes, subterranean aquifers, and solution mining (14). Sodium is found in large quantities in most areas of the world. Its quantity is so large that prices in some locations are only a few dollars per ton. Many areas have millions of tons but prices are so low that it is not economical to mine or process the salt. The largest exposed sodium chloride bed is at the Salat de Uyuni, Bohvia, but Bohvia is landlocked and very htde of the salt can be processed and sold at a profit. 

Term extraction and analysis software, in patent searching, 18 244 Terminal model theory, 29 832 Terminal activity coefficients, 8 743 Terminal lakes... 

Further classification of lakes relates to their position within the regional groundwater-flow system. Terminal-lake systems are defined as lakes that function as the discharge point of the regional groundwater-flow system. For terminal lakes, water is removed by evaporation and sometimes through surface outflow. These lakes typically evolve into saline lake systems characteristic of the semiarid or arid regions of the world (32). 

Currently, typical trifluoroacetic acid concentrations in surface water range from approximately 100 to 500 ng/1, although trifluoroacetic acid concentrations as great as 6.4 xg/l have been found in certain terminal lakes [237,239]. 

Areally close compositional contrast is seen in the recent rift area of Djibouti. On the western border, the terminal Lake Abhe is fed by the sodium-carbonate-type Awash River from the Ethiopian volcanic highlands, whereas the Asal Lake near an arm of the Gulf of Aden is fed by seawater through recent fault zones and hydrothermal inputs in addition to local runoff, and precipitates halite and gypsum (Fontes et al., 1979). 

N13P HBKF-A Total height 240 mm over standard terminal lake-off cell box height 216 mm ... 

An in ilial assuni ption is th at the reaction Lakes place with maxi-rn tint overlap between the HOMO on on e rn oleculc an d th e I.L MO on the other, fti e HOMO of ph en ylbuLadiene h as m ost den sity on the terminal carhon atom. 

In the third e.vample, the line terminates at 53%. This means DO NOT run this pump at less than 53% of the BEP. 53% of 4500 gpm is 2385 gpm. Because this is a firewater pump and because firemen need to throttle the nozzles on their fire hoses, then we need to install a pressure relief valve on this system with a discharge bypass line so that the pump dumps the restricted water (less than 2400 gpm) back into the suction tank or lake. If not, this firewater pump is likely to suffer bearing failure during an emergency. 

Mirex has been detected in air, surface water, soil and sediment, aquatic organisms, and foodstuffs. Historically, mirex was released to the environment primarily during its production or formulation for use as a fire retardant and as a pesticide. There are no known natural sources of mirex and production of the compound was terminated in 1976. Currently, hazardous waste disposal sites and contaminated sediment sinks in Lake Ontario are the major sources for mirex releases to the environment (Brower and Ramkrishnadas 1982 Comba et al. 1993). 

For many years, petroleum and heavy oil were very generally defined in terms of physical properties. For example, heavy oil was considered to be a crude oil that had gravity between 10 and 20° API. For example. Cold Lake heavy crude oil (Alberta, Canada) has an API gravity equal to 12°, but extra-heavy oil (such as tar sand bitumen), which requires recovery by nonconventional and nonenhanced methods, has an API gravity in the range 5 to 10°. Residua would vary depending on the temperature at which distillation was terminated, but vacuum residua were usually in the range 2 to 8° API. 

Phelps TJ, Zeikus JG. 1984. Influence of pH on terminal carbon metabolism in anoxic sediments from a mildly acidic lake. Appl Environ Microbiol 48 1088-95. 

Ochre is very common in the Terminal Archaic-Early Formative archaeological site of Jiskairumoko, (Rio Have, Lake Titicaca Basin, southern Peru). Within the site, ochre was found on tools, palettes, and in burials and soil deposits within structures in several contexts, suggesting both symbolic and functional uses of ochre. Variations in the color and contexts imply possibilities for different uses of ochre.. Instrumental neutron activation analysis was used to analyze the ochre samples found in Jiskairumoko. Multivariate analysis of the elemental data by principal components analysis suggests trends in the data related to the compositional variation of ochres on the site. Further analysis of the ochre will lead to conclusions about the variation in composition of the ochres from Jiskairumoko and possible archaeological conclusions about ancient technologies and uses of ochre on the site. 

To localize ERp on paraffin sections, 65-kDa antirat ER antibodies are used (Upstate Biotechnology, Lake Placid, NY). This antibody is obtained by immunizing rabbits with synthetic peptides representing the N-terminal amino acid residues 46-63 of human ER(3. The deparaffinized sections on slides are placed in the Target Retrieval Solution (pH 6.1)... 

---