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Slope field

Upland. Grown in level to steeply sloping fields that are rarely flooded. No effort is made to impound water as for other rice ecosystems. Crop is direct seeded on ploughed dry soil or dibbled in wet, non-puddled soil. [Pg.4]

Soil erosion, therefore, is the greatest threat to the economic and environmental sustainability of United States agriculture (Mueller, 1995). Pimentel et al. (1995) concluded that soil erosion is a major environmental and agricultural problem worldwide, and efforts to reduce these losses must be supported. Erosion rates have exceeded replacement values on most sloping fields since the Europeans introduced plowing and grain farming as North America was settled. [Pg.522]

Harford panted behind me. Certainly, we have not been idle, although we came prepared—we had been given a sketch of what was required. And as I say, your husband... so clear about what he wanted. Do you remember there is a painting in your London residence, a landscape by Lorrain, an idyll of woods, sloping fields, water, and human habitation in the classic style When we saw the lie of the land, the position of the... [Pg.87]

As a first step, we plot the slope field for the system in the (r,x) plane (Figure 2.8.2), Here the equation x = x(l - x) is being interpreted in a new way for each point (r.x), the equation gives the slope dx/dt of the solution passing through that point. The slopes are indicated by little line segments in Figure 2.8.2. [Pg.35]

Slope field) The slope is constant along horizontal lines in Figure 2.8.2. Why should we have expected this ... [Pg.42]

Sketch the slope field for the following differential equations. Then integrate the equation manually by drawing trajectories that are everywhere parallel to the local slope. [Pg.42]

MaSTERSON, W. D. 2001. Petroleum filling history of central Alaskan North Slope Fields. PhD Dissertation, University of Texas at Dallas. [Pg.87]

In the majority of schools, accommodation is adequate, but in a significant minority of schools the lack of a school hall, deteriorating hard areas, sloping fields or poor drainage restrict proper development of physical education. [Pg.96]

The known oil and gas reservoirs on the North Slope fields are shown in Figure 3. Oil and gas occurs over a wide area at various horizons. Source rock was abundant in Paleozoic and Upper Cretaceous/Tertiary to generate sufficient quantity of hydrocarbons to fill traps of various resrvoirs. Gas from Paleozoic Package occurs in Triassic Sadlerochit Formation near Barrow In the east. In Kemik and Kavik in the west, and In Seal Island, and Gwydyr Bay in the north. Lower Cretaceous gas have been observed in Prudhoe Bay complex, Kuparuk, Milne Point, Point Thomson and the Beaufort-Mackenzie areas, Canada in the east. [Pg.141]

That the use of North Slope gas for the enhanced oil recovery on the North Slope fields is the best option. [Pg.153]

On sloping fields, problems can arise with run-off if water is applied too quickly. It may run down between potato ridges, for example, without really wetting the ridges where the crop roots are growing. There is less run-off if a bed system is used (see "The bed system" subsection in Section 15.3.6). [Pg.205]

The slope of the expectation curve indicates the range of uncertainty In the parameter presented a broad expectation curve represents a large range of uncertainty, and a steep expectation curve represents a field with little uncertainty (typical of fields which have much appraisal data, or production history). [Pg.161]

Introduction and commercial application Investment opportunities in the exploration and production (E P) sector of oil and gas business are abundant. Despite areas such as the North Sea, Gulf of Mexico and the North Slope in Alaska being mature areas, there are still many new fields under development in those regions, and new areas of business interest are opening up in South America, Africa and South East Asia. Some fields which have a production history of decades are being redeveloped, such as the Pedernales Field in Venezuela. [Pg.303]

Plotting r versus 1/n gives kTJqJ as the intercept and (kTJqJ)( -y) as the slope from which and y can be determined. Figure A2.3.29 illustrates the method for lattices in one, two and tliree dimensions and compares it with mean-field theory which is independent of the dimensionality. [Pg.543]

Example For the AMEER force field, a carbonyl C-0 bond has an eqnilibrniin bond length of 1.229 A and a force con stant of 570 kcal/mol A-. The potential for an aliphatic C-C bond has a in ini-mum at 1.526 A. I hc slope of the latter poten tial is less steep a C... [Pg.23]

The slope of the hysteresis loop in is also an important parameter. From this slope, the parameter S can be derived (17). In Figure 3 a part of the hysteresis loop (M as a function of the appHed field H) is given. The point at which M is constant as the function of the appHed field is defined as saturation magnetisation (M.). From the slope at can be written tan0 = = 1/ 1 — S ) ot dM/dH = — S ). Thus the S is defined in... [Pg.172]

The other refining centers in the United States are all located near one of the major pipelines that are suppHed either from the Gulf Coast oil fields or from Oklahoma, Texas, or Louisiana fields. The Pacific Northwest refineries were originally suppHed mostly by Canadian production. Currently (ca 1995), these refineries are predominantly suppHed by Alaskan North Slope cmde, which is brought in from Valdez to the refinery ports in tankers. [Pg.87]

Fig. 2. Electron drift velocities as a function of electric field for A, GaAs and B, Si The gradual saturation of curve B is characteristic of all indirect semiconductors. Curve A is characteristic of direct gap semiconductors and at low electric fields this curve has a steeper slope which reflects the larger electron mobiUty. The peak in curve A is the point at which a substantial fraction of the electrons have gained sufficient energy to populate the indirect L minimum which has a much larger electron-effective mass than the F minimum. Above 30 kV/cm (not shown) the drift velocity in Si exceeds that in... Fig. 2. Electron drift velocities as a function of electric field for A, GaAs and B, Si The gradual saturation of curve B is characteristic of all indirect semiconductors. Curve A is characteristic of direct gap semiconductors and at low electric fields this curve has a steeper slope which reflects the larger electron mobiUty. The peak in curve A is the point at which a substantial fraction of the electrons have gained sufficient energy to populate the indirect L minimum which has a much larger electron-effective mass than the F minimum. Above 30 kV/cm (not shown) the drift velocity in Si exceeds that in...
Fig. 12. Log—log plot of current density,/, versus appHed electric field, E, for a ZnO varistor at room temperature, ia which the breakdown field. Eg, is iadicated. The exponent d equals the iaverse slope of the curve, log Ej J) = 1/a, and is a measure of device nonlinearity. Units of current density and the... Fig. 12. Log—log plot of current density,/, versus appHed electric field, E, for a ZnO varistor at room temperature, ia which the breakdown field. Eg, is iadicated. The exponent d equals the iaverse slope of the curve, log Ej J) = 1/a, and is a measure of device nonlinearity. Units of current density and the...

See other pages where Slope field is mentioned: [Pg.270]    [Pg.522]    [Pg.106]    [Pg.58]    [Pg.212]    [Pg.291]    [Pg.270]    [Pg.522]    [Pg.106]    [Pg.58]    [Pg.212]    [Pg.291]    [Pg.311]    [Pg.914]    [Pg.415]    [Pg.531]    [Pg.617]    [Pg.1561]    [Pg.2892]    [Pg.21]    [Pg.75]    [Pg.510]    [Pg.369]    [Pg.428]    [Pg.1]    [Pg.48]    [Pg.312]    [Pg.411]    [Pg.135]    [Pg.350]    [Pg.365]    [Pg.222]    [Pg.229]    [Pg.238]    [Pg.362]   
See also in sourсe #XX -- [ Pg.35 ]




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