Experimental technique on infrared radiation in wake of blunt cone in high-enthalpy tunnel

介绍在JF-10氢氧爆轰驱动高焓激波风洞中开展再人流场红外辐射测量的实验技术。风洞试验状态的驻室总压为19．6MPa，驻室总温为7920K。实验以球头钝锥体为试验模型，测量其近尾流红外辐射能量通量的横向分布。测量采用插入式锑化铟多元红外成像系统，波段范围为2．27-6．0μm。试验数据呈现明显的规律性。试验结果表明：利用这一测量技术能够提供高焓条件下有较高空间分辨率的、较为准确的红外实验数据

法学家眼中的和谐社会

从现有权威性文献看,“和谐社会”是执政党要追求的一种社会状态,更是一种涉及面极其广泛的治国方略。在这个过程中,法律、法学和法学家的作用举足重轻。面对如此重大议题,法学家应当表达观点、提出诉求、发挥专业功能。基于这种考虑,本刊特邀部分中青年法学家进行了笔谈,希望他们的文章能引起讨论,促进法律界、法学界形成一些基本共识

EXPERIMANTAL RESEARCH ON INFRARED RADIATION IN HYPERSONIC FLOW AROUND BLUNT CONE

报道了在JF-10氢氧爆轰驱动高焓激波风洞中开展的再入流场红外辐射实验研究，风洞的试验状态为：驻室总压19．6MPa，总焓15．5MJ／kg，自由流速度约5km／s，实验以锑化铟多元红外成像系统为测量手段，以球头钝锥体为试验模型，测量激波层与近尾流中红外辐射功率的横向分布剖面，试验数据呈现明显的规律性，试验结果表明，激波层内壁面附近的红外辐射功率较小，中间有一区域辐射较大且相对均匀，激波层外缘辐射单调减小；尾流中红外辐射功率在轴线附近的核心区最大，随着离轴线距离的增大而单调减小

高超声速钝锥流场红外辐射实验研究

报道了在JF-10氢氧爆轰驱动高焓激波风洞中开展的再入流场红外辐射实验研究，风洞的试验状态为：驻室总压19．6MPa，总焓15．5MJ／kg，自由流速度约5km／s，实验以锑化铟多元红外成像系统为测量手段，以球头钝锥体为试验模型，测量激波层与近尾流中红外辐射功率的横向分布剖面，试验数据呈现明显的规律性，试验结果表明，激波层内壁面附近的红外辐射功率较小，中间有一区域辐射较大且相对均匀，激波层外缘辐射单调减小；尾流中红外辐射功率在轴线附近的核心区最大，随着离轴线距离的增大而单调减小

活性炭在中高温条件下对玉米秸秆厌氧发酵的影响

为提高玉米秸秆厌氧发酵的产气效果,本文研究活性炭在中温(38℃)和高温(50℃)条件下对玉米秸秆厌氧发酵产甲烷的效果及微生物学机制.结果表明,添加活性炭能显著促进秸秆厌氧发酵产甲烷,中、高温试验组(添加活性炭)的累积产甲烷量分别比对照提高了63%和96%;DGGE的结果显示,高温试验组(添加活性炭)和对照组(未添加活性炭)的发酵液中的优势细菌菌群分别是Clostridiale bacterium和Bacillus,中温对照组发酵液和中温试验组发酵液未发现明显优势菌种.添加活性炭分别有利于氢营养型的甲烷鬃毛菌(Methanosaeta concilii strain)和乙酸营养型的醋酸甲烷八叠球菌(Methanosarcina acetivorans strain),在中温、高温试验组的发酵液中形成优势古菌菌群.中温试验组活性炭载体上的优势古菌菌群为甲烷鬃毛菌(Methanosaeta concilii strain),而高温试验组活性炭载体上的优势古菌菌群主要为甲烷八叠球菌嗜高温菌属(Methanosarcina thermophila strain)

城市土地价格调查、评价及动态监测

<p>本书是国内第一本以实证研究为主，全面介绍城市土地价格调查、评价和动态监测研究的专著。在城市土地定级途径的选择、分类定级研究重点确定、城市土地定级与城市规划研究的关系上，有独到的见解；按照城市地价的区域表现形式，提出了基本地价区片、地价区片和读地定级单元的基准递加测算办法。通过对递加评估方法、土地收益还原率、递加修正系数等深入研究，阐明了机遇基准地价进行标定评估的价格修正体系建立的依据与方法。围绕城市土地价格动态监测的目标和任务，对城市地价标准宗地的选择、地价指数的编制、地价信息的发布、查询及应用等问题进行了研究。</p><p>本书适于国土资源、土地管理、不动产价格评估、城市规划和经济管理专业的科研、教学人员和相关部门的管理干部学习和参考。</p><p>&nbsp;</p

EFFECTS OF TIDAL CREEK MORPHOLOGY ON SPATIAL DISTRIBUTION OF SOIL ORGANIC CARBON IN SOIL IN TIDAL WETLAND

Soil organic carbon is a major carbon pool in tidal wetland ecosystems. By dividing the level of the tidal creek and calculating its morphological characteristic index, the spatial distribution characteristics of the typical tidal creek system were analyzed, taking a typical natural tidal channel as the research object. The spatial distribution characteristics of soil organic carbon were analyzed by geostatistical methods. In addition, the effects of morphological characteristics of the tidal creek on the spatial distribution of soil organic carbon were explored. The results showed that there was obvious spatial heterogeneity in the morphological characteristics of the tidal creek. In the middle tidal flats, the connectivity of the tidal creek network was higher, and the density, curvature and bifurcation ratio were also higher than that in other tidal zones. The tidal creek length gradually increased with the increase of tidal creek development grade, while the tidal creek curvature gradually decreased with the increase of tidal creek development grade. The spatial interpolation results showed that the lowest soil organic carbon in 0 to 10 cm soil layer occurred in the middle tidal flats where tidal creeks were more developed, and within the 10~ 20 cm soil layer, soil organic carbon showed a gradually increasing trend from sea to land, and showed a strip-shaped spatial distribution choracteristic. In the low tidal flats, the mean value of soil organic carbon in a third-order creek was significantly greater than that in a first-order creek. In the middle tidal flats, the mean value of soil organic carbon in a second-order creek was significantly greater than that in a third-order and a first-order creek. The soil organic carbon of the high tide flats was not significantly correlated with the tide creek development level. Within the 0 to 10 cm soil layer, the soil organic carbon gradually increased with increasing distance to the tidal creek in low and middle tidal flats. Within the 10 to 20 cm soil layer, the soil organic carbon gradually decreased with increasing distance to tidal creek in the middle tidal flats. However, there was no correlation between the soil organic carbon and the distance to the tidal creek in high tidal flats. The spatial heterogeneity in the morphological characteristics of the tidal creek was one of the important factors of spatial differences in soil organic carbon content in the tidal wetland. Therefore, morphology changes in tidal creeks should be considered in order to accurately estimate the soil carbon pools in tidal wetlands