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Underground existence

The volume of the freshwater amounts to only one-thirtieth of the 1.25 x 10 km (300 x 10 mi ) of the water ia salty oceans. Approximately one-third of the freshwater exists permanently as snow and ice (3). A large portion of the remaining freshwater has infiltrated too far underground or is partially polluted with minerals and chemicals and therefore is not readily usable. The entire life system on the earth depends on the remaining freshwater sources therefore, it is essential to protect the quaUty of the available waters. [Pg.220]

The problem of permeability exists whenever a plastic material is exposed to vapor, moisture, or liquids. Typical cases are electrical batteries, instruments, components installed underground, encapsulated electrical components, food packaging, and various fluid-material containers. In these cases, a plastic material is called upon to form a barrier either to minimize loss of vapor or fluid or to prevent the entrance of vapor or fluid into a product. From the designers viewpoint, the tolerable amount of permeation established by test under conditions of usage with a prototype product of correct shape and material is the only direct answer. [Pg.308]

Sulfur is a yellow, relatively low melting solid. Traditionally it has been obtained from underground deposits where it is melted in place with steam and then pumped out in a fairly pure state. Newer sources are metal ores or natural gas where the sulfur exists in a chemically combined state. [Pg.18]

Natural attenuation relies on natural processes to clean up or attenuate pollution in soil and ground-water. Natural attenuation occurs at most polluted sites. However, the right conditions must exist underground to clean sites properly. If not, cleanup will not be quick enough or complete enough. Scientists monitor or test these conditions to make sure natural attenuation is working. This is called monitored natural attenuation (MNA)94-96... [Pg.643]

The hydrosphere (the Greek prefix hydro means water) is the great mass of water that surrounds the crust of the earth. Water is one of a few substances that, at the temperatures normal on the surface of the earth (which range between about -50 and 50°C), exists in three different states liquid, gas, and solid. Liquid water makes up the oceans, seas, and lakes, flows in rivers, and underground streams. Solid water (ice) occurs in the polar masses, in glaciers, and at high altitudes, and gaseous water (moisture) is part of the atmosphere (O Toole 1995). Liquid and solid water cover over 70% of the surface of the earth. [Pg.436]

Steinhausler (1987) and Martell (1987) review the dosimetric models and related model studies. Their view is that there are still very large uncertainties in the existing data and in the extrapolation from the exposure and response data for underground miners and experimental animals to the health effects of the radon progeny levels to which the general public is exposed. B.L. Cohen (1987) describes his work to relate radon measurements with lung cancer rates for various geographical areas to test the concept of a dose threshold. [Pg.11]

All use of chlordane was banned in Norway in 1967 (Ingebrigtsen et al. 1984). In August 1975, the USEPA issued its intent to suspend registrations and prohibit production of all pesticides containing heptachlor or chlordane, based on evidence of carcinogenicity (Glooschenko and Lott 1977). On July 1, 1983, chlordane use was prohibited in the United States for any purpose except to control underground termites. A similar situation exists in Japan (Ohno et al. 1986 Tojo et al. 1986). [Pg.874]

Natural Gas - A mixture of hydrocarbon compounds and small amounts of various nonhydrocarbons (such as carbon dioxide, helium, hydrogen sulfide, and nitrogen) existing in the gaseous phase or in solution with crude oil in natural underground reservoirs. [Pg.287]

The underground tanks at this site were located in a tank hold that extended into the shale. When the release occurred, gasoline migrated downward into the shale and groundwater. Groundwater in the shallow aquifer in this area is not used, due to limited quantity and poor quality, although a significant concern existed due to elevated hydrocarbon vapors. A local basement fire had been attributed to the presence of the vapors. [Pg.315]


See other pages where Underground existence is mentioned: [Pg.131]    [Pg.131]    [Pg.423]    [Pg.423]    [Pg.429]    [Pg.454]    [Pg.358]    [Pg.155]    [Pg.524]    [Pg.127]    [Pg.78]    [Pg.958]    [Pg.958]    [Pg.363]    [Pg.670]    [Pg.40]    [Pg.158]    [Pg.17]    [Pg.32]    [Pg.340]    [Pg.13]    [Pg.132]    [Pg.629]    [Pg.693]    [Pg.1046]    [Pg.477]    [Pg.43]    [Pg.591]    [Pg.591]    [Pg.28]    [Pg.239]    [Pg.832]    [Pg.1661]    [Pg.226]    [Pg.215]    [Pg.160]    [Pg.77]    [Pg.69]    [Pg.187]    [Pg.483]    [Pg.33]    [Pg.162]   
See also in sourсe #XX -- [ Pg.25 ]




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