八单元一维位置灵敏雪崩室

In the experiment of nuclear reaction, it is important to measure the mass, charge, energy and emitted direction of particles. For multiparameter measurement, we must use a detector or a group of detectors which can give the time, energy, and position information. The Large Area position sensitive Ionization Chamber(LAIC) is one of the eight experiment terminals of HIRFL. It is built for researching nuclear reactions from low energy to intermediate energy. It is an excellent equipment for energy measurements and atomic number identification of emitted fragments in this energy region. It is also designed to give the time and position information of the emitted fragments by itself. Obviously, an IC can not supply a good timing signal. Moreover, the mechanical installation is different from the original design by some other reasons. In this case, it is not enough to obtain the correct direction information of the emitted fragments. To obtain good timing signals and the correct direction information, some modifications must be made. It is well known that a PPAC can give us excellent timing signals. It also can be easily built as a position sensitive detector. For this reason, a specially designed PPAC is installed in the entrance of the LAIC. For the different purposes, two types of PPACs were designed and tested. Both are OCTPSACs (OCTunit one dimension Position Sensitive Avalanche Counter). In this paper, both OCTPSACs will be introduced. Based on the requirements of the LAIC, the OCTPSACs consist of eight position sensitive PPACs. Each PPAC has an anode and a cathode. In both cases, the sizes are same. But different type of cathodes are used. In one type of OCTPSAC, its cathode is made of wire plane. It consists of gold-plated tungsten wires with the diameter of 20μm, spaced 0.5 mm apart from each other. The anode is a mylar foil which was evaporated by gold layer with the thickness of 50μg/cm~2 mounted on a printed plate in the shape of rectangle. the thickness of mylar foil is 1.5μm. The gap between anode and cathode is 3mm. The performance of the OCTPSAC has been tested by using a ~(252)Cf source in flowing isobutylene gas at the pressure of 3.4mb. The intrinsic time resolution of 289ps and position resolution of 2 mm have been obtained. In another type of OCTPSAC, the cathode is made of mylar foil, which is composed of gold strip by vacuume evaporation method with a special mask on the mylar foil. The thickness and the width of the gold strip is 50μg/cm~2 and 1.7mm. The strips are spaced 0.3 mm apart from each other. The anode is the same as the former type. We have obtained the time resolution of 296ps and position resolution of 2mm by using ~(241)Am-a source when the gas pressure is 6 mb and high voltage is 600V. The working gas is heptane

1∶50万SOTER制图与数据采集——以辽河下游地区为例

本文阐述辽河下游地区 1∶5 0万SOTER建立中SOTER图编制与数据采集的过程及有关问题 .

长白山地区近50年平均最高和最低气温变化

利用线性趋势法对长白山地区13个气象台站建站以来的逐日温度资料进行分析,确定该区域的气温变化趋势,同时通过Mann-Kendall方法确定突变点位置,并结合t检验法进行检验。结果表明:区域的年平均最高气温和最低气温都有极为显著的增加趋势,分别为每10年增加了0.23和0.46℃(α=0.001);近50年的最高气温和最低气温的时间系列都有一个突变点,其中最高气温的突变点出现在1995年左右,最低气温的突变点在1985年前后。这种变化使得温度日较差表现出明显的减小趋势,并在1972年出现一个突变点,前后平均相差0.8℃。区域各月最高、最低气温及气温日较差与日照百分率均有极为显著的相关关系,一定程度上反映了温室效应持续增强的迹象。

延安市近50年来降水特征及趋势变化的小波分析研究

利用Morlet小波对延安1952~2003年52年间的降水量进行了多时间尺度分析,结果表明,延安降水在3~6 a和25~32 a的时间尺度上变化较强,存在近22 a和3 a的降水周期,其中22 a的周期变化最为强烈。根据降水周期,延安年降水在2003年后的5~8 a内相对偏多,2007~2009年左右达到最大值,然后降水量开始减少,从2013年左右开始进入一个约10 a的少雨阶段。基于1952~1990年降水量资料,建立小波变换的最近邻抽样回归模型,用1990~2003年13 a的年降水量变化作为校验,13年中有11年的预测结果相对误差小于30%,说明小波分析和最近邻抽样回归模型结合可以较好地预测降水量的年际变化。

近50年北京植被对全球变暖的响应及其时效:基于遥感数据和物候资料的分析

植被对全球变暖的响应方式及其程度问题是全球变化研究的焦点之一。利用1951～2000年的气温、降水等气候资料、1982～2000年的NOAA/AVHRR遥感数据和1951～2002年山桃始花的物候数据,分析了北京各气候参量与生态系统植被在年际和年内时间尺度上的变化规律及其关系。结果表明,北京近20年增温12℃,增温态势显著;过去50年中,降水的年际变化小于生长季内的波动幅度。年NDVI最大值(VP)、平均值(VM)的年际变化曲线呈波动中缓慢上升的趋势,表明植被的生长状况总体上在变好或生长季在延长。VP出现

玛纳斯河流域50年绿洲扩张及生态环境演变研究

玛纳斯河流域绿洲开发和经济发展是新疆维吾尔自治区的典范,以不同时相的卫星影像、土地利用图和地形图为数据源,借助遥感和地理信息系统等先进技术,恢复了玛纳斯河流域过去50年来6个时期(1949,1962,1976,1989,1999和2001年)的绿洲分布格局和动态演化过程.研究表明,按照绿洲年扩张速率,该流域的绿洲扩张过程可分为两个阶段:1949~1976年为绿洲化阶段,因人口急剧增加,耕地面积急剧扩大,绿洲总面积从1949年的156.385km2扩张到1976年的3639.491km2;1976~2001

The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP

Planktonic foraminiferal delta O-18 record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chinese loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, correlating to Gothenburg, Mungo and Laschamp events, approximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The delta O-18 curve of the Okinawa Trough is well associated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the prominent regional controlling factor.