工业“物”语:沈阳地区工业博物馆藏品的界定

沈阳工业正经历一场调整、转变、发展的重大变革,保护、改造与再利用这些珍贵的工业文明遗存成为人们普遍关注的热点。博物馆无疑成为一支重要的力量,在保护工业遗存、传承工业文明、展示工业文化方面发挥着作用。藏品是博物馆的核心内容,博物馆的一切工作都围绕着'物'而展开。工业博物馆藏品的收藏、研究及展示工作,都应该在合理的、全面的藏品体系下,得以顺利开展。在系统梳理沈阳工业发展历史的基础上,借助博物馆学有关'物'的研究理论。

Effect of Different Temperatures on Microbes and Its Quality of Green Pepper During Circulation

[Objective] The aim was to study on effect of different temperatures on microbes and its quality of green pepper during circulation. [Method] Measurement was conducted on change of colibacillus, salmonella, Listeria number, and its quality of green pepper stored at 9 and 20 ℃ respectively. The green peppers stored at 9 ℃ for 16 d were under simulated sale. In addition, effects of microbe number of green peppers stored at 20 ℃ for 4 d by different washing methods were measured. [Result] Indices of green pepper were different when green peppers were stored for 16 d at 9 ℃ and sold at 20 ℃ after 16 d storage. Specifically, under the former condition, sensory quality, weight-loss rate, Vc content, chlorophyll content and soluble protein were 4.1, 1.79%, 95.6, 20.3, and 93.3 mg/100 g; under the latter condition, the corresponding indices were 3.3, 3.87%, 81.2, 16.5, 85.6 mg/100 g, respectively. Colibacillus numbers for green pepper stored 16 d at 9 ℃, sold for 1 d at 20 ℃ after 16 d storage and stored for 4 d at 20 ℃ were 46, 3.2×103 and 3.1×104 cfu/g; during the test, salmonella and Listeria were not found; colibacillus in green pepper could be eliminated by 1×10-3 ml/L of chloros and most colibacillus in green pepper could be cleared away by 1 drop/L of detergent and running water. [Conclusion] Stored at 9 ℃, quality of green pepper could be better preserved and colibacillus propagation could be controlled.

Compound-specific δD and its hydrological and environmental implication in the lakes on the Tibetan Plateau

The hydrogen isotopic composition(δD) of n-alkanes in lacustrine sediments is widely used in palaeoenvironmental studies, but the heterogeneous origins and relative contributions of these lipids provide challenges for the interpretation of the increasing dataset as an environment and climatic proxy. We systematically investigated n-alkane δD values from 51 submerged plants(39 Potamogeton, 1 Myriophyllum, and 11 Ruppia), 13 algae(5 Chara, 3 Cladophora, and 5 Spirogyra) and 20 terrestrial plants(10 grasses and 10 shrubs) in and around 15 lakes on the Tibetan Plateau. Our results demonstrate that δD values of C_(29) nalkane are correlated significantly with the lake water δD values both for algae(R^2=0.85, p<0.01, n=9) and submerged plants(R^2=0.90, p<0.01, n=25), indicating that δD values of these algae and submerged plants reflect the δD variation of lake water. We find that apparent hydrogen isotope fractionation factors between individual n-alkanes and water(εa/w) are not constant among different algae and submerged plants, as well as in a single genus under different liminological conditions, indicating that the biosynthesis or environmental conditions(e.g. salinity) may affect their δD values. The δD values of submerged plant Ruppia in the Xiligou Lake(a closed lake) are significant enriched in D than those of terrestrial grasses around the lake(one-way ANOVA,p<0.01), but the algae Chara in the Keluke Lake(an open lake) display similar δD values with grasses around the lake(one-way ANOVA, p=0.826>0.05), suggesting that the n-alkane δD values of the algae and submerged plants record the signal of D enrichment in lake water relative to precipitation only in closed lakes in arid and semi-arid area. For each algae and submerged plant sample, we find uniformed δD values of different chain length n-alkanes, implying that, in combination with other proxies such as Paq and Average Chain Length, the offset between the δD values of different chain length n-alkanes can help determine the source of sedimentary n-alkanes as well as inferring the hydrological characteristics of an ancient lake basin(open vs closed lake).

Electrical conductivities of two granite samples in southern Tibet and their geophysical implications

There are clear differences in the electrical conductivities of the crustal granites of the Qinghai-Tibet Plateau.Because these granites are among the major rock types on the Qinghai-Tibet Plateau, it is very important to detect the electrical conductivity of granites under high temperatures and pressures to study the electrical conductivity structure of this area. Using impedance spectroscopy at a frequency range of 10.1–106 Hz, the electrical conductivity of the muscovite-granite collected from Yadong was investigated at a confining pressure of 1.0 GPa and temperatures ranging from 577 to 996 K, while the electrical conductivity of the biotite-granite collected from Lhasa was investigated at a pressure of 1.0 GPa and temperatures ranging from587 to 1382 K. The calculated activation enthalpies of the Yadong muscovite-granite sample is 0.92 eV in the low-temperature range(577–919 K) and 2.16 eV in the high-temperature range(919–996 K). The activation enthalpies of the Lhasa biotite-granite sample is 0.48 eV in the low-temperature range(587–990 K) and 2.06 eV in the high-temperature range(990–1382 K). The change in the activation enthalpies of the granites at different temperature ranges may be associated with the dehydration of the two samples. The electrical conductivities of the granite samples obtained in the laboratory using impedance spectroscopy correspond well with field observations conducted near the sampling points, both in terms of the actual conductivity values and the observed variations between the low-temperature and high-temperature regimes. This correlation of laboratory and field conductivities indicates that the conductivities of the crustal rocks in the two regions closely correspond to granite conductivities.We calculated the electrical conductivities of muscovite-granite and biotite-granite samples using the effective medium and HS boundary models. When applied to the crustal rocks of southern Tibet, the results of the geophysical conductivity profiles lie within the range of laboratory data. Thus, the electrical characteristics of the crustal rocks underlying the southern Qinghai-Tibet Plateau can largely be attributed to granites, with the large changes to high conductivities at increasing depths resulting from the dehydration of crustal rocks with granitic compositions.