On the basis of the analysis and study of the records of shallow-layer profiles and information from systematic analyses of some cores and their 14C datings, the sediments of Yellow Sea trough since the final slage th...On the basis of the analysis and study of the records of shallow-layer profiles and information from systematic analyses of some cores and their 14C datings, the sediments of Yellow Sea trough since the final slage the Late Pleistocene are found to have the following features. On the south slope of the trough, it is probably composed of island-shelf de posits. On the mouth of the trough, it is made up of eolian dunes and its deposits. In the centra! bottom region of the trough where intense desertization occurred in the early stage of the regression, there are parallel oblique beddings in the strata known as the 'angle of repose' texture, which demonstrates that the deposits there are composed of eolian sands. And in the late stage, thin derivative deposits developed in the northern part of the trough. On the north slope of the trough, thick-layer derivative deposits developed. This primary sedimentary pattern still remains unchanged since the occurrence of the Holocene transgression.展开更多
Salinity is an important property of industrial and natural waters. It is defined as the measure of the mass of dissolved salts in a given mass of solution. High salinity has an impact on people and industries reliant...Salinity is an important property of industrial and natural waters. It is defined as the measure of the mass of dissolved salts in a given mass of solution. High salinity has an impact on people and industries reliant on water. High levels of salt can reduce crop yields, limit the choice of crops that can be grown and, at higher concentrations over long periods, can kill trees and make the land unsuitable for agricultural purposes. Salinity increases the “hardness” of water, which can mean more soap and detergents have to be used or water softeners installed and maintained. This can also cause scaling in pipes and heaters. The experimental determination of the salt content by drying and weighing presents some difficulties due to the loss of some components. The only reliable way to determine the true or absolute salinity of natural water is to make a complete chemical analysis. However, the method is time consuming and cannot yield the precision necessity for accurate work. Thus to determine salinity, one normally used method involves the measurement of a physical property such as conductivity, density or refractive index. The paper reports the refractometric fiber optic sensor for detection of salinity of water. The mathematical model is developed for detection of the refractive index of liquid and simulated in MATLAB. The fiber optic sensor probe is developed to measure the refractive index of the solution containing different amount of salt dissolved in water i.e. different molar concentrations. Experiments are carried out using the developed probe for these solutions. Experimental results are showing good agreement with the simulated results.展开更多
基金Project sponsored by the State Natural Sciences Foundation of China
文摘On the basis of the analysis and study of the records of shallow-layer profiles and information from systematic analyses of some cores and their 14C datings, the sediments of Yellow Sea trough since the final slage the Late Pleistocene are found to have the following features. On the south slope of the trough, it is probably composed of island-shelf de posits. On the mouth of the trough, it is made up of eolian dunes and its deposits. In the centra! bottom region of the trough where intense desertization occurred in the early stage of the regression, there are parallel oblique beddings in the strata known as the 'angle of repose' texture, which demonstrates that the deposits there are composed of eolian sands. And in the late stage, thin derivative deposits developed in the northern part of the trough. On the north slope of the trough, thick-layer derivative deposits developed. This primary sedimentary pattern still remains unchanged since the occurrence of the Holocene transgression.
文摘Salinity is an important property of industrial and natural waters. It is defined as the measure of the mass of dissolved salts in a given mass of solution. High salinity has an impact on people and industries reliant on water. High levels of salt can reduce crop yields, limit the choice of crops that can be grown and, at higher concentrations over long periods, can kill trees and make the land unsuitable for agricultural purposes. Salinity increases the “hardness” of water, which can mean more soap and detergents have to be used or water softeners installed and maintained. This can also cause scaling in pipes and heaters. The experimental determination of the salt content by drying and weighing presents some difficulties due to the loss of some components. The only reliable way to determine the true or absolute salinity of natural water is to make a complete chemical analysis. However, the method is time consuming and cannot yield the precision necessity for accurate work. Thus to determine salinity, one normally used method involves the measurement of a physical property such as conductivity, density or refractive index. The paper reports the refractometric fiber optic sensor for detection of salinity of water. The mathematical model is developed for detection of the refractive index of liquid and simulated in MATLAB. The fiber optic sensor probe is developed to measure the refractive index of the solution containing different amount of salt dissolved in water i.e. different molar concentrations. Experiments are carried out using the developed probe for these solutions. Experimental results are showing good agreement with the simulated results.
