JFET SOS devices: Processing and gamma radiation effects

A process for fabricating n channel JFET/SOS (junction field-effect transistors on silicon-on-sapphire) has been researched. The gate p(+)n junction was obtained by diffusion, and the conductive channel was gotten by a double ion implantation. Both enhancement and depletion mode transistors were fabricated in different processing conditions. From the results of the Co-50 gamma ray irradiation experimental we found that the devices had a good total dose radiation-hardness. When the tot;ll dose was 5Mrad(Si), their threshold voltages shift was less than 0.1V. The variation of transconductance and the channel leakage current were also little.

Measurement of the isospin-filtering dd → 4He K+K- reaction at Q = 39 MeV

The total cross-section for the dd → 4HeK+K− reaction has been measured at a beam momentum of 3.7GeV/c, corresponding to an excess energy of 39MeV, which is the maximum possible atthe Cooler Synchrotron COSY-Jülich. A deuterium cluster-jet target and the ANKE forward magnetic spectrometer, placed inside the storage ring, have been employed in this investigation. We find a total cross-section of σtot < 14 pb, which brings into question the viability of investigating the dd → 4He a0(980)reaction as a means of studying isospin violation.

CSR外靶实验终端大型探测器读出电子学研制

兰州重离子加速器-冷却储存环外靶实验终端大型探测器中子墙和TOF墙分别共有504个和360个通道用于测量中子和带电粒子的飞行时间,需要高精度时间测量的读出电子学系统。研制的8通道读出电子学模块采用了前沿定时的时间测量方法、基于TOT技术的电荷测量方法和PXI总线平台,电子学测试结果显示时间测量精度好于25ps。

dd→αK+K-反应截面在ANKE/COSY上的测量

ANKE谱仪是位于冷却储存环COSY上的一个内靶实验终端，在它的针对物理目标中，研究靠近 产生阈的共振态a0(980)/f0(980)是一个主要的内容。在通过强相互作用反应对a0/f0进行测量时，初态会选择使用不同的同位旋组合，也就是使用pp、 pn、pd和dd反应。本实验完成于2006年的4、5月间，是一个使用COSY所能提供的最大束流动能Td = 2.273 GeV的dd道反应，它比 产生阈高Q = 39 MeV。在实验中探测了αK+符合事件，结合使用丢失质量分析方法就可以对反应链dd → αf0 → αK+K- 以及其中的f0(980)共振态进行研究。 作为本文的主要内容这个实验，是在Monte - Carlo模拟的帮助下准备后，在4个星期的束流时间里完成的。在实验完成后，数据分析主要集中在对稀有的αK+事件进行鉴别。 ANKE的射程望远镜阵列针对K+介子的鉴别做过优化，在它的帮助下K+就可以通过飞行时间、能量损失方法，以及探测延迟发射的K+衰变产物而被挑选出来。而与之关联的α粒子则是通过它们相对于K+介子的定时点进行鉴别的，α和K+的动量及轨迹由在相应多丝正比室上测量到的径迹信息重建。由此，就可以通过使用丢失质量方法鉴别出实验中没有测量的K-介子。最终所得的αK+丢失质量谱在K-介子质量区域内呈现一个峰，其中包含大约15个事件。由这些αK+K-事件可以得到总的反应截面σtot = (9 ± 3sta ± 5sys) pb。 同位旋破缺反应dd → α(π0η) 的截面由测量得到的σtot (dd → αK+K-)值推出，进而它也给出了在WASA-at-COSY上观察这个过程所要求的最短束流时间。因为这个反应被认为主要是源于通过KK中间态的f0 → a0转化，所以它对于确定出轻标量介子a0(980)/f0(980)的结构扮演着格外重要的角色

Geochemical properties of the variolitic andesite from Susong in the Dabie orogenic belt, China

The variolitic andesite from the Susong County in the Dabie Mountains implies that it was erupted in water. The mineralogy of the varioles is primarily radiate plagioclase (albite sind oligoclase), with little pyroxene, hornblende and quartz (derived from alteration). The pyroxene, hornblende and quartz are in the interstices between plagiocalse. The matrix consists of glass, hornblende, chlorite, epidote and zoisite. It is clearly subjected an extensive alteration. The andesite has an uncommon chemical composition. The SiO2 content is about 56.8%, TiO2 = 0.9%, MgO = 6.4%, Fe2O3 (tot) = 6.7%similar to 7.6%, 100Mg/(Mg + Fe) = 64.1 similar to 66.2. Mg-# is significantly high. The andesite has high abundances of large-lithophile trace elements (e.g. K, Ba. Sr, LREE), e.g. La/Nb = 5.56 similar to 6.07, low abundances of high-strength-field elements (HFSE e.g. Ta, Nb, P, Ti), particularly Ta and Nb strongly depleted. These are consistent with the characteristics of subduction-related magmas. In the spider diagram of trace elements, from Ce to right hand, the abundances of elements decrease quickly, showing a character of the continental margins. There has a strong punishment of light-rare-earth elements, with a significant diffraction of REEs (the mean value of (La/Yb)(N) is 32.84). No Eu anomaly, but there are anomaly high (La/Yb)(N) = 28.63 similar to 36.74, (La/Y)(N) = 70.33 similar to 82.4. The elements Y and Yb are depleted greatly, Y<20 g/g, Y-N = 2.74 similar to 2.84, Yb-N = 2.18 similar to 2.35. From the La-(La/Sm) diagram, the andesite is derived from partial melting. But the epsilone value of Nd is - 18.7 similar to -19.2, so that the material source may be the mantle materials affected by the crustal materials. The Nd model age is 1.9 Ga indicating that the variolitic basaltic andesite was resulted from the mantle wedge of North China block, which had the Nd model age of 2.5Ga, when the Yangze block which had the Nd model age of 1.7Ga subducted beneath it. So the variolitic andesite has characteristics of the island-are volconic rocks oil a continental basement in the vicinity of the destructive continental margin.