Preliminary study on climatic signals of stable isotopes from Holocene speleothems under monsoon condition

Within the East Asian monsoon zone the change in oxygen isotope of Holocene stalagmite is mainly related to monsoon rain rather than to temperature. And carbon isotope can be taken as a comprehensive signal which contains the natural information and the information of anthropogenic activity. Isotopic analysis is also compared with the annual layer records.     

沥青砂浆粘弹性断裂扩延分析及其断裂特性的推求

以沥青砂浆材料为例,通过薄板的蠕变断裂及单轴拉伸蠕变的试验结果和数据分析,推求出沥青砂浆在不同温度下的断裂特性参数Γ和σｍＩ１。     

Search for new antiphytovirucides

The lead compound of substituted 2-(4′-hydroxyphenyl)benzimidazoles were modified by phosphorylation sulfonation and carboxymethylation. The benzimidazoloamidophosphate (6) (7) have better activity against tobacco mosaic virus (TMV). The benzimidazolophenoxyacetic acid, phenoxysulfonic acid containing trifluoromethyl, and nitro group have 77%≈85% efficiency for wheat rust disease. Supported by the National Natural Science Foundation of China and National Laboratory of Elemento Organic Chemistry Nankai University Qu Fanqi: born in 1952, Associate professor     

水合氯化铜和8—羟基喹啉固相配位反应的热化学研究

用自行研制的具有恒定温度环境的新型反应热量计,以３ｍｏｌ．Ｌ＾－１ＨＣｌ溶液为量热溶剂,在２９８．２Ｋ条件下,测定了配合物Ｃｕ（ＨＱ）Ｃｌ２的标准生成焓,其值为：－３４０．３０ｋＪ．ｍｏｌ＾-１。     

利用真实砂岩微观孔隙模型研究粘性不稳定指进

利用真实砂岩微观孔隙模型进行了不同油水粘度比下的油水两相驱替试验,研究了粘性不稳定指进;提出了控制注入水粘性指进的注入速度及油水粘度比的要求,对指导油田生产有一定的意义。     

一种高效覆盖的节点放置算法

提出了一种新的高效覆盖的节点放置方法．该算法的目的是使传感器的数目最优化，并确定能支持分布式传感器网络的传感器的配置，其基本思路是剔除局部冗余，提升整体性能．最后通过仿真与已有的算法进行比较，展示了其性能的优越性．     

高纯部分稳定二氧化锆微粉的制备工艺

高纯Zr02微粉作为高温高强特种陶瓷和耐火材料等的重要原料，由于晶型转变所引起的体积效应而影响其耐高温性能，限制其应用范围，因此必须进行晶型稳定化处理．本文介绍了以氧化钇为稳定剂的高纯部分稳定二氧化锆微粉的制备技术及产品质量标准．     

几丁质酶基因在转基因烟草中表达效率的检测

采用氨基葡萄糖法检测转基因烟草植株叶片几丁质酶活力，结果表明几丁质酶基因在转基因植株中酶活力增强，与β—1,3-葡聚糖酶基因的协同作用下酶活性最强，几丁质酶活力的测定对外源基因表达效率的检测是可行的．     

Paleotemperature changes ver the past 3000 years in eastern Beijing, China:A reconstraction based on Mg/Sr records in a stalagmite

The Mg/Sr ratio in a stalagmite, which is directly proportional to DMg/Ca, the solid-liquid distribution coefficient of Mg, is proposed as a geochemical thermometer to estimate paleotemperature changes. The paleotemperature changein eastern Beijing over the past 3000 years has been reconstructed by using this thermometer in the stalagmite ZFFS-1 from Jingdong Cave. The records can be divided into two periods: 3000-2000 aBP, cool and wet, the air temperature averaging 9.8℃; and 2000 aBP-present, hot and dry, the air temperature being 1℃ higher than the mean value (11.7℃) of the past 3000 years. During 500-200 aBP, the air temperature was about 1.2℃ lower than that of the present, corresponding to the Little Ice Age in Europe. Like δ18O and δ13C, Mg/Sr (or DMg/Ca) reflects an obviously warming trend of the past 200 years. These results are supported by historic records.