应用量子力学

本书是为电工和力学工程师、材料科学家和应用物理学家而编写的。书中材料虽取自量子力学理论书，但应用于实际，采用了实际工程的例子、练习和工作解法。内容从经典力学和电磁学出发，发展到现代量子力学及其应用。     

Isotopic evidence for the moisture origin and composition of surface runoff in the headwaters of the Heihe River basin

We investigated the moisture origin and contribution of different water sources to surface runoff entering the headwaters of the Heihe River basin on the basis of NECP/NCAR (National Centers for Environmental Prediction/National Center for Atmospheric Research) re-analysis data and variations in the stable hydrogen and oxygen isotope ratios (?? D and ?? ¹⁸O) of precipitation, spring, river, and melt water. The similar seasonality in precipitation ?? ¹⁸O at different sites reveals the same moisture origin for water entering the headwaters of the Heihe River basin. The similarity in the seasonality of ?? ¹⁸O and d-excess for precipitation at Yeniugou and Urumchi, which showed more positive ?? ¹⁸O and lower d-excess values in summer and more negative ?? ¹⁸O and higher d-excess values in winter, indicates a dominant effect of westerly air masses in summer and the integrated influence of westerly and polar air masses in winter. Higher d-excess values throughout the year for Yeniugou suggest that in arid inland areas of northwestern China, water is intensively recycled. Temporal changes in ?? ¹⁸O, ??D, and d-excess reveal distinct contributions of different bodies of water to surface runoff. For example, there were similar trends for ?? D, ?? ¹⁸O, and d-excess of precipitation and river water from June to September, similar ?? ¹⁸O trends for river and spring water from December to February, and similar trends for precipitation and runoff volumes. However, there were significant differences in ?? ¹⁸O between melt water and river water in September. Our results show that the recharge of surface runoff by precipitation occurred mainly from June to mid-September, whereas the supply of surface runoff in winter was from base flow (as spring water), mostly with a lower runoff amount.     

Epitaxial growth of ultrathin ZrO2（111） films on Pt（111）

Ordered epitaxial ZrO2 films were grown on Pt(111) and characterized by low energy electron diffraction (LEED), synchrotron radiation photoemission spectroscopy (SRPES) and X-ray photoelectron spectroscopy (XPS). The films were prepared by vapor deposition of zirconium in an O2 atmosphere followed by annealing under ultra high vacuum. At low coverages, the films grew as discontinuous two-dimentional islands with ordered structures. The size and structure of these islands were dependent on the coverage of Zr...     

Comparative genomic analysis reveals more functional nasal chemoreceptors in nocturnal mammals than in diurnal mammals

Natural selection has a critical role in the diversity of morphological traits. However, the genetic basis underlying the evolution and diversity of morphological characteristics, particularly in the context an organism’s behavior, lifestyle, and environment, is not well understood. The discovery of nasal chemoreceptors in mammals provided an opportunity to address this question. Here, we identify 4 nasal chemoreceptor gene families (V1R, V2R, OR, and TAAR) from horse, guinea pig, marmoset and orangutan genome sequences, respectively. Together with previously described mammalian nasal chemoreceptor gene repertoires, we found a significant positive correlation between functional gene number and morphological complexity, both in the main olfactory system and the vomeronasal system. The combined analysis of morphological data, behavioral data, and gene repertoires suggests that nocturnal mammals tend to possess more species-specific chemoreceptor genes and more complicated olfactory organs than diurnal mammals. Moreover, analysis of evolutionary forces revealed the existence of positive selection on the species-specific genes, likely reflecting the species-specific detection of odors and pheromones. Taken together, these results reflect a rare case of adaptation to circadian rhythm activity at the genome scale, and strongly suggest that the complexity of morphological olfactory organs and the diversification of nasal chemoreceptors in nocturnal mammals are under selection for the ability to perceive the variety of odors that nocturnal mammals may encounter in their particular dark environments.     

Relationship between climatic conditions and the relative abundance of modern C3 and C4 plants in three regions around the North Pacific

Using −24‰ and −14‰ as the endpoints of stable carbon isotopic composition of total organic carbon (δ¹³C_TOC) of surface soil under pure C₃ and C₄ vegetation, and surface soil δ¹³C_TOC data from eastern China, Australia and the Great Plains of North Amer- ica, we estimate the relative abundance of C₃/C₄ plants (i.e., the ratio of C₃ or C₄ biomass to local primary production) in modern vegetation for each region. The relative abundance of modern C₃/C₄ vegetation from each region is compared to the corresponding climatic parameters (mean annual temperature and precipitation) to explore the relationship between relative C₄ abundance and climate. The results indicate that temperature controls the growth of C₄ plants. However, even where temperature is high enough for the growth of C₄ plants, they will only dominate the landscape when precipitation declines as temperatures increase. Our results are consistent with those of other investigations of the geographic distribution of modern C₄ plant species. Therefore, our results provide an important reference for interpretation of past C₃/C₄ relative abundance records in these three regions.     

Isotopic evidence for the moisture origin and composition of surface runoff in the headwaters of the Heihe River basin

We investigated the moisture origin and contribution of different water sources to surface runoff entering the headwaters of the Heihe River basin on the basis of NECP/NCAR(National Centers for Environmental Prediction/National Center for Atmospheric Research) re-analysis data and variations in the stable hydrogen and oxygen isotope ratios(δ D and δ 18O) of precipitation,spring,river,and melt water. The similar seasonality in precipitation δ 18O at different sites reveals the same moisture origin for water ...     

Is the maximum carbon number of long-chain <Emphasis Type="Italic">n</Emphasis>-alkanes an indicator of grassland or forest? Evidence from surface soils and modern plants

The molecular distribution of long-chain n-alkanes in 62 soil samples collected from diverse locations across eastern China was analyzed.The long-chain n-alkanes were mostly dominated by n-C29 or n-C31,regardless of the overlying vegetation type at each site.The results were compared with those summarized from the literature,covering more than 100 soil samples within China and more than 300 genera of modern plants distributed worldwide.There were similar n-alkane distribution patterns for most genera, with no clear differences among grasses,shrubs,and trees.The evidence from analyses of surface soils and modern plants indicates that the relationship between the molecular distribution of long-chain n-alkanes of surface soils and source vegetation is highly complex,and is influenced by many factors.Further,it is suggested that source vegetation types should not be simply inferred from distribution patterns of long-chain n-alkanes in sediments.     

Comparison of the carbon isotope composition of total organic carbon and long-chain <Emphasis Type="Italic">n</Emphasis>-alkanes from surface soils in eastern China and their significance

Surface soil samples collected over a high spatial resolution in eastern China were analyzed for carbon isotope composition （δ^13C） of total organic carbon （TOC） and higher plant-derived long-chain n-alkanes, with the latter reported as weighted mean values. The two sets of δ^13C values are significantly correlated and show similar trends in spatial variation. The spatial distribution of δ^13C shows less negative values in the mid-latitudes between 31°N and 40°N and more negative ones at higher and lower latitudes. This is consistent with previously reported carbon isotope data from surface soil phytoliths in the same region and suggests that the mid-latitude area provides relatively favorable growing condi- tions for C4 plants. Furthermore, δ^13C values of both TOC and long-chain n-alkanes from 12 surface soil samples collected from a small grassland in north China displayed similar carbon isotope values and the difference between paired δ^13C of a soil samples remains relatively constant. Our data demonstrate that in eastern China, soil δ^13C composition of both TOC and long-chain n-alkanes is effective indicators of C3/C4 ratios of the prevailing vegetation. This work suggests that -22‰ and -32‰ are good es- timated end members for the weighted mean δ^13C values of long-chain n-alkanes （C27, C29 and C31 n-alkanes） from soils under dominant C4 or C3 vegetation, allowing us to reconstruct paleovegetation trends.