Lanthanide Ionization Energies and the Sub-Shell Break. Part 2. The Third and Fourth Ionization Energies

By interpolating a 4fq6s → 4fq7s transition within the sequence f1 → f14 rather than between f0 and f14, revised third and fourth ionization energies of the lanthanides have been obtained. The revised values, together with the second ionization energies calculated in a previous paper, are used to calculate values of the standard enthalpies of formation of the gaseous tripositive ions, ΔfHƟ(M3+,g), and of the lattice and hydration enthalpies of some lanthanide compounds and ions in the trivalent and tetravalent states. The displacements of f0 values from nearly smooth f1 → f14 variations exceed 30 kJ mol-1 and indicate substantial subshell breaks

Valencies of the lanthanides

The valencies of the lanthanides vary more than was once thought. In addition to valencies associated with a half-full shell, there are valencies associated with a quarter- and three-quarter-full shell. This can be explained on the basis of Slater’s theory of many-electron atoms. The same theory explains the variation in complexing constants in the trivalent state (the “tetrad effect”). Valency in metallic and organometallic compounds is also discussed

VALUE-ADDED ACTIVITIES AS A RURAL DEVELOPMENT STRATEGY

Community/Rural/Urban Development,

Crambe as a Specialty Crop in North Dakota

Production Economics,

Rural Land-Use Trends in the Conterminous United States, 1950-2000.

In order to understand the magnitude, direction, and geographic distribution of land-use changes, we evaluated land-use trends in U.S. counties during the latter half of the 20th century. Our paper synthesizes the dominant spatial and temporal trends in population, agriculture, and urbanized land uses, using a variety of data sources and an ecoregion classification as a frame of reference. A combination of increasing attractiveness of nonmetropolitan areas in the period 1970–2000, decreasing household size, and decreasing density of settlement has resulted in important trends in the patterns of developed land. By 2000, the area of low-density, exurban development beyond the urban fringe occupied nearly 15 times the area of higher density urbanized development. Efficiency gains, mechanization, and agglomeration of agricultural concerns has resulted in data that show cropland area to be stable throughout the Corn Belt and parts of the West between 1950 and 2000, but decreasing by about 22% east of the Mississippi River. We use a regional case study of the Mid-Atlantic and Southeastern regions to focus in more detail on the land-cover changes resulting from these dynamics. Dominating were land-cover changes associated with the timber practices in the forested plains ecoregions and urbanization in the piedmont ecoregions. Appalachian ecoregions show the slowest rates of landcover change. The dominant trends of tremendous exurban growth, throughout the United States, and conversion and abandonment of agricultural lands, especially in the eastern United States, have important implications because they affect large areas of the country, the functioning of ecological systems, and the potential for restoratio

Science, Measurement, and Technology Requirements for Infrared Climate Benchmark Missions

Quantifying climate change in the presence of natural variability requires highly accurate global measurements covering more than a decade. Instrument design considerations for trending terrestrial emitted radiance are described

Physiography of Nares Strait: importance to the origin of the Wegener Fault

Nares Strait is a long, deep trough which, at its shoreline at least, is straight. Most theories of its origin are deduced from observations remote from the Strait and even those observations adjacent to the Strait were seldom if ever taken for the express purpose of elucidating its origin. Direct observations of the floor of the Strait are very scarce, yet without them the dilemma of movement or non-movement seems unresolvable. We have been able to map the gross physiography of the Strait and can deduce from it that the area has undergone compression along an approximately northwest-southeast axis. In order to resolve the dilemma of motion or no motion along Nares Strait, we suggest that a post-Palaeozoic northward movement (50-100 km) of the Canadian Arctic Islands by the process of crustal thinning in Lancaster and Jones Sounds and in the Sverdrup Basin can, when combined with geologic/geometric uncertainties, account for the present-day relatively small observed net offset