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Location of wells

Other information that can be obtained from such map is the location of faults, the status and location of wells and the location of the fluid contacts. Figure 5.45 shows some of the most frequently used map symbols. Structural maps are used in the planning of development activities such as well trajectories/targets and the estimation of reserves. [Pg.140]

Diagram of county landfill showing the location of wells used to monitor groundwater. [Adapted from R-C. Li and R. Rojagopol, Am. Environ. Lab. October 1994,... [Pg.663]

Correct molecular structures are dependent on the proper location of wells in the PES, so they are intimately related to the energetics of conformational analysis. For organic molecules, most gross structural details are modeled with a reasonable degree of accuracy. Dewar, Jie, and Yu (1993) evaluated AMI and PM3 for 344 bond lengths and 146 valence angles... [Pg.139]

Figure 2. Location of wells, Rock Springs site 4... Figure 2. Location of wells, Rock Springs site 4...
Figure 6. Location of wells, Green River site 1... Figure 6. Location of wells, Green River site 1...
Figure 2-4 Iso-lines on the top of Middle Eocene and location of wells at Ninotsminda, Tbilisi Area... Figure 2-4 Iso-lines on the top of Middle Eocene and location of wells at Ninotsminda, Tbilisi Area...
Figure 30.3 Location of wells in the USGS midwestern groundwater monitoring network. (A) Location of wells (mostly drinking water) sampled in the USGS midwestern groundwater monitoring network during 1991-1994. (B) Location of municipal drinking water wells sampled in Iowa during 1995-1998. Figure 30.3 Location of wells in the USGS midwestern groundwater monitoring network. (A) Location of wells (mostly drinking water) sampled in the USGS midwestern groundwater monitoring network during 1991-1994. (B) Location of municipal drinking water wells sampled in Iowa during 1995-1998.
Thirty crude oils from the BCF were collected (1) along two parallel and generally southwest-northeast trends. The areal extent of the BCF showing locations of wells sampled is shown in Figure 1. These oils were characterized by their API gravity, percent saturates, aromatics, NSO and asphaltene compounds, gas chromatograms for whole oils, CA-C7 fractions, and aromatics. Concurrently, 24 associated waters were also sampled and analyzed for Ca++, Mg++, Na+, HC03, C03 , SOA , pH, and total dissolved solids (TDS) (1). [Pg.593]

Figure 1. Areal extent of Bolivar Coastal Fields showing locations of wells sampled (Reprinted with permission from Ref, 1. Copyright 1983 Bockmeulen et al.)... Figure 1. Areal extent of Bolivar Coastal Fields showing locations of wells sampled (Reprinted with permission from Ref, 1. Copyright 1983 Bockmeulen et al.)...
Answer 4.4 The fault in Fig. 4.6 was plotted on the basis of abrupt changes in recorded lithologies between wells 6 and 7 (Table, Fig. 4.6a). An alternative interpretation The calcareous sandstone was deposited on a limestone relief with a steep paleo-erosional face between the locations of wells 6 and 7. [Pg.422]

Figure 1 Map showing the location of wells and directions of groundwater flow. Snake River Plain aquifer, Idaho... Figure 1 Map showing the location of wells and directions of groundwater flow. Snake River Plain aquifer, Idaho...
Figure 4 Map showing the prepumping potentiometric surface of the Floridan aquifer and locations of wells shown... Figure 4 Map showing the prepumping potentiometric surface of the Floridan aquifer and locations of wells shown...
Figure 5 Cross-section showing location of wells and concentrations of dissolved solids in the Floridan aquifer... Figure 5 Cross-section showing location of wells and concentrations of dissolved solids in the Floridan aquifer...
Fig. 1. Main structural features of the southwestern Barents Sea, and locations of wells used in the present study. Geology after Gabrielsen et al. (1990). Fig. 1. Main structural features of the southwestern Barents Sea, and locations of wells used in the present study. Geology after Gabrielsen et al. (1990).
Yerevan water supply aqueduct feed only groundwater bodies related to fractured basalts, and analyses of wells cross-sections indicate that water body in the location of wells 3, 11 are not overlaid by impermeable strata. And it is strongly recommended to limit economic activities in these locations. [Pg.47]

Fig. 2. Simplified map of the study area showing major structural features of the Oseberg field and location of wells sampled. The dashed line A-B corresponds to the position of the geological cross-section shown in Fig. 3. Fig. 2. Simplified map of the study area showing major structural features of the Oseberg field and location of wells sampled. The dashed line A-B corresponds to the position of the geological cross-section shown in Fig. 3.
Fig. 4. (a) Seismic travel-time structure map showing surface of Lower Cretaceous limestone marker in the Hibernia Anticline and location of wells used in this study. From Arthur el a . (1982). (b) Schematic cross-section along line A-A (corresponding to zone 2 in Fig. 3), showing three main reservoir sandstones of Hibernia Field Avalon, B ... [Pg.366]

Figure 2, Grid used in the modeling simulation. Locations of wells used in the model calibration are also shown. The shaded area designates the portion of the field treated with aldicarb in 1979-80. Figure 2, Grid used in the modeling simulation. Locations of wells used in the model calibration are also shown. The shaded area designates the portion of the field treated with aldicarb in 1979-80.
Fig. 39 Location of wells used in second phase of block-cyclic-steaming of petroli.ferous formation. Wells 1-production 2-injection 3-abandoned 4-observation S-stnicture contours drawn on top of massive carbonate bed (contour figures indicate depths measured from a surface datum level). Fig. 39 Location of wells used in second phase of block-cyclic-steaming of petroli.ferous formation. Wells 1-production 2-injection 3-abandoned 4-observation S-stnicture contours drawn on top of massive carbonate bed (contour figures indicate depths measured from a surface datum level).
Transmissivity of an aquifer may place a limit on the safe yield, even though this equation may indicate a potentially large draft. This can only be realised if the aquifer is capable of transmitting groundwater from the source area to the wells at a rate high enough to sustain the draft. Where the pollution of groundwater is possible, then the location of wells, their type... [Pg.189]

Fig. 8. Index map of the Gippsland Basin, showing basin location, tectonic setting (the graben represented by the two platforms and the Central Deep), major structures, and location of well. (After Weeks and Hopkins 1967 Hocking 1972 Bodard et al. 1984)... Fig. 8. Index map of the Gippsland Basin, showing basin location, tectonic setting (the graben represented by the two platforms and the Central Deep), major structures, and location of well. (After Weeks and Hopkins 1967 Hocking 1972 Bodard et al. 1984)...

See other pages where Location of wells is mentioned: [Pg.187]    [Pg.197]    [Pg.373]    [Pg.150]    [Pg.24]    [Pg.202]    [Pg.250]    [Pg.162]    [Pg.76]    [Pg.253]    [Pg.136]   
See also in sourсe #XX -- [ Pg.403 , Pg.412 ]




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