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Analysis of Nonmetric Theories of Gravity .1. Electromagnetism
(1983-1983)
No abstract available.
Analysis of Nonmetric Theories of Gravity .3. Summary of the Analysis and its Application to Theories in the Literature
(1983-1983)
No abstract available.
Natural emissions of chlorine-containing gases: Reactive Chlorine Emissions Inventory
(1999-04)
Although there are many chlorine-containing trace gases in the atmosphere, only those with atmospheric lifetimes of 2 years or fewer appear to have significant natural sources. The most abundant of these gases are methyl ...
Schiff Conjecture on Gravitation
(1982-1982)
No abstract available.
Schiff Conjecture on Gravitation - Respond
(1983-1983)
No abstract available.
Nucleotide sequence, genomic organization and evolution of a major repetitive DNA family in tilapia (Oreochromis mossambicus/hornorum )
(1989)
A highly repetitive DNA sequence from tilapia (Oreochromis mossambicus/hornorum ) has been cloned and sequenced. It is a tandemly arrayed sequence of 237 bp and constitutes 7% of the fish genome. The copy number of the ...
A new measurement of CO sub(2) eddy flux in the nearshore atmospheric surface layer
(1991)
Fluxes of CO sub(2) in the atmospheric surface layer have been measured at a shoreline site by the eddy correlation method using a new CO sub(2) sensor with greater sensitivity than the ones used in earlier studies. In ...
Explanation for the 4.8-V plateau LiCrxMn2-xO4
(1998-03)
No abstract available.
Ocean-atmosphere exchange of methyl bromide: NW Atlantic and Pacific Ocean studies
(1998-07)
Measurements of methyl bromide partial pressure and concentration in surface water and air samples in the NW Atlantic Ocean in July 1995 and the Pacific Ocean in October 1995 are presented, Mean atmospheric mixing ratios ...
Effect of the nonlinearity of the carbonate system on partial pressure of carbon dioxide in the oceans
(1995-04)
Partial pressure of CO sub(2) is a nonlinear function of several seawater properties. Due to the nonlinearity in this relationship, the partial pressure of a uniform ocean would be different from that of a nonuniform ocean ...