五种化学品对鱼类的毒性效应

本文以鱼类为试验材料,对五种化学品(TNT废水,DE添加剂,N_-,503,松根油,“孑孓灵”制剂)进行了毒性试验和评价。结果表明,TNT废水对鲫鱼的96小时的LC_(50)值为2.1mg/L,而且还引起鱼的肝组织细胞的胀肿等病变;DE添加剂对草鱼种的96小时的LC_(50)值为6.1mg/L;N-503(纯品)、工业品和N-503加煤油对白鲢鱼种的96小时的LC_(50)值分别为0.2,0.8和1.26mg/L;松根油,丁黄药对麦穗鱼48小时的TLm值为27.8mg/L和222mg/L,松根油和丁黄药混

地下结构的爆炸振动效应与冲击破坏行为研究

对爆源近区地下混凝土管道结构在爆炸冲击载荷作用下的动力学响应开展探索性实验研究。选用钢筋混凝土管道模拟地下结构，尺寸为：$\phi_{\hbox{内}}$800mm$\times$2000mm$\times$100mm。通过实验研究定量确定爆炸振动波载荷对地下结构产生的振动效应；定性确定爆炸冲击波载荷对地下管道结构和混凝土材料产生的动态破坏效应。爆炸当量分别为50 g和100 g TNT，爆炸距离取为0.1，0.3，1，7和10m。实验主要涉及地下管道结构在小药量爆炸点近区的破坏效应与爆炸药量和爆炸距离间关系的确定；混凝土材料破坏行为与药量和爆炸距离关系的确定；爆炸冲击波的影响范围以及爆炸振动波的有效影响范围与爆源特性的关系及爆炸响应函数的确定。从小当量地下结构爆炸实验观察到：地下结构的爆炸振动响应，即振动波波长和频率不同于土介质地表的波长和频率。与地表面上建筑物的波长和频率相比，振动波长持续作用时间明显缩短，且振动频率显著提高。这与地下结构的爆炸动力学响应，特别是爆源近距离的结构动力学响应存在着本质的区别。不同的爆炸距离和当量，地下爆炸对地下结构可以产生振动和冲击两种不同特征的动力学效应。在折算距离大于0.22$\sim$0.25 m/W$^{1/3}$时，100 g TNT当量的爆炸以产生振动效应为主。在折算距离小于0.22$\sim$0.25 m/W$^{1/3}$时，爆炸主要产生冲击效应；在爆炸距离小于1.5m/W$^{1/3}$时，地下爆炸振动波对结构产生的动力学响应的明显特征是管道结构发生径向变形。而且，管道上与爆源最近点是管道变形的对称点。管道的轴向和环向动力响应表现为相应方向上的刚体振动。在爆炸距离大于1.5 m/W$^{1/3}$，如等于2.15m/W1/3的情况下，爆炸振动波对管道结构产生的动力学响应主要表现为整体振动。结构的变形特征基本消失；地下爆炸冲击波载荷对爆源近区管道结构和混凝土材料可以产生三种破坏效应：在折算距离等于0.065 m/W$^{1/3}$时，低强度的冲击波载荷仅产生结构破坏效应。实验中观察到混凝土管道只沿其轴线方向上形成贯穿性裂纹，管道内外表面均无损伤和破碎现象；当折算距离等于0.027 m/W1/3时，较强冲击波载荷既引起管道的结构破坏，也产生混凝土材料的破坏。这时观察到沿混凝土管道轴线方向上，以及与轴线成30$^\circ$至50$^\circ$范围内形成贯穿性裂纹。同时在管道内表面出现直径约为210 mm的层裂区，最大层裂厚度约为8$\sim$12 mm；当折算距离等于0.022 m/W$^{1/3}$时，爆炸强冲击波载荷主要引起的混凝土材料破坏形式表现为破碎。即在管道上以爆源最近点为中心形成直径约为370 mm的贯穿性孔洞，还观察到该孔洞周边不同方向上有长度为230$\sim$410 mm不等的数条细裂纹形成。

新型固定式烧毁炉系统研究

介绍了一种新型的固定式烧毁炉系统,该系统主要用于装药量100gTNT当量以下的非金属外壳防步兵地雷以及火工品的烧毁处理。通过PLC的自动控制,实现了烧毁处理过程的自动协调控制;同时,配备了视频监控系统,使烧毁工作更安全可靠。本设计完全满足工艺要求,实际应用中提高了工作效率。

山东西部中生代碳酸岩和火山岩的地球化学特征及其成因研究

On account of some very peculiar features, such as extremely high Sr and Nd contents which can buffer their primary isotopic signatures against crustal contamination, deep-seated origin within mantle, and quick ascent in lithosphere, carbonatites are very suitable for deciphering the nature of sub-continental lithospheric mantle(SCLM) and receiving widespread attentions all around the world. The Mesozoic carbonatites located in western Shandong was comprehensively investigated in this dissertation. The extremely high REE concentrations, similar spider diagrams to most other carbonatites around the world and high Sr. low Mn contents of apatite from carbonatites confirm their igneous origin. The K depletion of carbonatites from this studies reflect the co-existing of carbonatite melts with pargasite+phlogopite lherzolite rather than phlogopite lherzolite. Geological characteristics and their occumng without associated silicate rocks argue against their origin of fractionation of or liquid immisibility with carbonated silicate melts. In contrast to the low S7Sr/86Sr and high l43Nd/l44Nd of other carbonatites in the world, carbonatites of this studies show EMU features with high S7Sr/86Sr and low l4jNd/144Nd ratios, which imply that this enriched nature was formed through metasomatism of enriched mantle preexisted beneath the Sino-korean craton by partial melts of subducted middle-lower crust of Yangtze craton. In addition to carbonatites, the coeval Mesozoic volcanic rocks from western Shandong were also studied in this dissertation. Mengyin and Pingyi volcanic rocks, which located in the south parts of western Shandong are shoshonite geochemically. while volcanic rocks cropped out in other places are high-K calc-alkaline series. All these volcanic rocks enriched in LREE and LILE. depleted in HFSE, and show TNT(strong negative anomalies in Ta, Nb. Ti) patterns in spider diagrams which are common phenomena in arc-related volcanic rocks. The Sr-Nd-Pb isotopic systematics reveal that the volcanic rocks decrease gradually in 87Sr/86Sr, 206Pb/204Pb, 20SPb/204Pb and increase in TDM from south to north, suggesting the distinction of SCLM beneath Shandong in Mesozoic is more explicit in south-north trending than in east-west trending. The variable features of SCLM can be attributed to the subduction of Yangtze craton beneath Sino-Korean craton, and subsequent metasomatism of SCLM by partial melts of Yangtze lower crust in different extent.