Adaptability of the u.s. Industrial relations system

An industrial relations system describes the basic values, laws, institutions, and organizational practices that govern employment relationships. To be effective, an industrial relations system must be well matched to its economic and social environment and able to meet the strategic needs of employers, the workforce, and the larger society. The current state of American industrial relations is assessed against these criteria. The general proposition advanced is that the U.S. system of industrial relations that grew out of the New Deal labor legislation of the 1930s performed effectively from the 1940s through the 1960s. Pressures for change on the system began to build through the 1970s because of changes in the economic and technological environment and in the strategic behavior and needs of the parties. These pressures erupted in the early 1980s to produce a period of experimentation and fundamental change in union-management relations. The critical question in industrial relations today is whether the process of adaptation will be sustained and expanded to cover a broader range of employment relationships.     

The "decade of the environment" in the u.s.s.R

The decade of the 1970's was for the U.S.S.R, as for the United States, a period of increased awareness of environmental deterioration. In response, new laws were passed, pollution control funding was increased, and natural resource conservation was heavily stressed. Despite such good intentions, the cumulative effects of new technologies, inadequate budgets and enforcement, the primacy of production goals, and various institutional impediments resulted in an uneven and in some places inadequate level of environmental enhancement.     

Energy and the u.s. Economy: a biophysical perspective

A series of hypotheses is presented about the relation of national energy use to national economic activity (both time series and cross-sectional) which offer a different perspective from standard economics for the assessment of historical and current economic events. The analysis incorporates nearly 100 years of time series data and 3 years of cross-sectional data on 87 sectors of the United States economy. Gross national product, labor productivity, and price levels are all correlated closely with various aspects of energy use, and these correlations are improved when corrections are made for energy quality. A large portion of the apparent increase in U.S. energy efficiency has been due to our ability to expand the relative use of high-quality fuels such as petroleum and electricity, and also to relative shifts in fuel use between sectors of the economy. The concept of energy return on investment is introduced as a major driving force in our economy, and data are provided which show a marked decline in energy return on investment for all our principal fuels in recent decades. Future economic growth will depend largely on the net energy yield of alternative fuel sources, and some standard economic models may need to be modified to account for the biophysical constraints on human economic activity.     

Military uses of uranium: keeping the u.s. Energy accounts

Present accounts of U.S. energy consumption are incomplete in two ways: they include neither the direct military uses of nuclear energy nor the mostly military, nonfuel uses of uranium. Preliminary estimates indicate that significant distortions are created in the data on U.S. nuclear energy consumption patterns as a result of these omissions.     

Radioactive wastes: a comparison of u.s. Military and civilian inventories

Contrary to widespread belief, the accumulated inventory of fission products generated by the still small U.S. civilian nuclear power industry may already be comparable to that generated in the past by U.S. military nuclear programs. Although the volumes of the military wastes are very large, they are on the average almost 100 times more dilute than projected commercial high-level wastes.     

Quaternary climates and sea levels of the u.s. Atlantic coastal plain

Uranium-series dating of corals from marine deposits of the U.S. Atlantic Coastal Plain coupled with paleoclimatic reconstructions based on ostracode (marine) and pollen (continent) data document at least five relatively warm intervals during the last 500,000 years. On the basis of multiple paleoenvironmental criteria, we determined relative sea level positions during the warm intervals, relative to present mean sea level, were 7 +/- 5 meters at 188,000 years ago, 7.5 +/- 1.5 meters at 120,000 years ago, 6.5 +/- 3.5 meters at 94,000 years ago, and 7 +/- 3 meters at 72,000 years ago. The composite sea level chronology for the Atlantic Coastal Plain is inconsistent with independent estimates of eustatic sea level positions during interglacial intervals of the last 200,000 years. Hydroisostatic adjustment from glacial-interglacial sea level fluctuations, lithospheric flexure, and isostatic uplift from sediment unloading due to erosion provide possible mechanisms to account for the discrepancies. Alternatively, current eustatic sea level estimates for the middle and late Quaternary may require revision.