The relationship between the temperature and the volume of a gas can be described by a certain function. Which of the following is most likely to be a function that represents this relationship? A. V = T + 5 B. V = T * 2 C. V = T^2 D. V = T / 3 相关知识点: ...
Exploring uncertainties in the relationship between temperature, ice volume, and sea level over the past 50 million years [1]聽Over the past decade, efforts to estimate temperature and sea level for the past 50 Ma have increased. In parallel, efforts to model ice sheet changes during this peri...
It was found that the data are consistent with a simple extension of the Flory-Huggins theory that accounts for finite volume changes of mixing.关键词: Polymer blends Mixing Pressure effects Gibbs free energy Mixtures Volume fraction Neutron scattering Approximation theory Temperature Mathematical models...
The pressure-volume-temperature(P-V-T) relationship of MgO has been calculated for conditions of high pressure(0～100 GPa) and high temperature(300～2000 K) using molecular dynamics simulations with the very similar potential models of Stoneham-Sangster and Lewis-Catlow.The results obtained have ...
This study was aimed to analyze the relationship between diameter at breast height, height, and volume of standing Shorea sp. and the relationship between age and volume of this species. The study was conducted at different ages of rehabilitated forest in Bintulu Sarawak, where the measurement ...
Hatch and Thomas D. Ruder - 《Forensic Science International》 被引量: 11发表: 2013年 [Studies on the estimation of the postmortem interval. 1. The temperature of cadaver (author's transl)] The relationship was investigated between the postmortem intervals and the rectal temperatures of 35 ...
Land surface temperature (LST) can reflect the land surface water-heat exchange process comprehensively, which is considerably significant to the study of environmental change. However, research about LST in karst mountain areas with complex topography i
(MIS1). The mildest glacial temperatures are reconstructed for the period between about 56 kyr ago and 26 kyr ago (that is, broadly coincident with MIS3), in agreement with the temperature histories of Greenland26and Antarctica27, and with the reduced volume of continental ice sheets ...
That water can exist in two distinct ‘glassy’ forms — low- and high-density amorphous ice — may provide the key to understanding some of the puzzling characteristics of cold and supercooled water, of which the glassy solids are more-viscous counterpa