带有噪声解耦的自校正解耦控制器

提出了一种不仅能够进行动静态解耦而且能够进行噪声解耦的自校正解耦控制器。在一定的条件下给出了稳定性和收敛性分析。通过仿真结果证明了给出算法的有效性。     

哀牢山与右江西部海西——印支期火山岩和板块构造环境

哀牢山和右江西部是华南板块古大陆边缘海西—印支期火山活动最频繁的地区之一。文章通过对该区火山岩的岩石学和地球化学综合分析,认为火山岩产于洋盆裂谷系、被动大陆边缘裂谷系、不成熟岛弧和弧后盆地裂谷系四种不同的板块构造环境中。有意义的是古特提斯洋板块相对华南板块于海西期扩张和印支期俯冲,哀牢山和右江西部的火山岩和板块构造环境出现相对应的同步演化关系。     

砂岩成岩作用的主要控制因素

侧重于宏观控制因素，强调了大地构造背景、盆地构造类型以及水溶液对砂岩成岩作用的影响，并指出深入探讨成岩作用与盆地类型和大地构造位置之间的关系，运用平衡热力学或溶液－矿物平衡知识研究成岩矿物相是成岩作用研究面临的更为复杂的任务。     

热连轧活套高度和张力系统的解耦控制

为了进一步提高板带热轧厂厚控精度及控制品质,需对具有非线性、强耦合、不确定、多约束特性的活套系统建立工程上适用的数学模型,以实现活套高度与张力系统的解耦控制.在分析其动态耦合过程的基础上,考虑到实际的活套系统在工作过程中变量的变化离其稳态工作点的偏差很小,以实际热轧现场数据为依据,给出了完整的传递函数表达形式.采用线性预测模型的BP神经网络PID控制策略以减弱系统的耦合影响,以提高控制效果.仿真结果验证了本算法的有效性,表明解耦后的活套控制系统可获得更好的控制效果.     

深部高应力松软岩层稳定性监测及实验研究

深部开采中巷道维护理论与浅部有十分明显的区别。这种差别的根源在于岩石赋存环境上的差异，尤其是深部高应力条件下岩石表现出十分特殊的力学行为。通过对宁夏石嘴山一矿38区＋600m轨道巷的工程地质调查、岩石力学实验、围岩变形与应力观测等，获得了宝贵的数据信息，为现场进行工业化试验和最终解决采掘接续和安全开采提供了科学依据。     

The evidence of fission-track data for the study of tectonic thermal history in Qinshui Basin

The thermal history of the Qinshui Basin has been studied by using the fission-track analysis of apatite and zircon, integrated analysis of tectonic evolution, magmatic activity and other palaeogeothermal analysis data. Results indicate that the palaeogeothermal gradient between the late-Paleozoic era and the medium-Mesozoic era is relatively low and the palaeogeothermal gradient in the late-Mesozoic is up to 5.56癈/100 m in the middle, and the values are relatively higher in the north and south margins of the basin, reaching over 8.00℃/100 m, which indicates that there was an anomalous tectonic thermal event in the thermal history of Qinshui Basin. This event happened in 110-140 Ma, and the main peak value was between 120 and 140 Ma. This anomalous tectonic thermal event is controlled by the strengthening thermal mobility of the lithosphere and magmatic intrusion. The maturity of the Permo-Carboniferous coal series mainly was controlled by this anomalous thermal field. The apatite fission track date of samples across the basin shows that a rapid tectonic uplifting with cooling existed 26.2-11.5 Ma ago and the upliftings in the north and south of the basin happened earlier than that in the middle. The Permo-Carboniferous strata had been completely annealed in the early 50 Ma, palaeotemperature over 125℃. Since then, especially from Oligocene-Miocene epoch, the strata which experienced large-scale tectonic upliftings with rapid cooling have been kept out of the annealing belt (70-125℃) in a relative low temperature environment. The late Mesozoic tectonic thermal event control hydrocarbon production peak (late Jurassic to early Cretaceous period) of Permo-Carboniferous strata in Qinshui Basin. When the strata experienced upliftings with rapid cooling since Oligocene-Miocene epoch, the hydrocarbon generation of coal series had stopped.     

Formation of the Yazi Spring Stream and its significance on tectonics-climate on the northern slope of Kunlun Mountains

The sequences of fluvial terraces in the Yazi Spring Stream are signs of the stepwise uplift of the Kunlun Mountains in the northern part of the Tibetan Plateau since the Late Pleistocene. Geomorphic and sedimentary features of the terraces reveal that they have resulted from the phased tectonic uplift and the consequent river incision in the northern plateau. Using the method of Single-aliquot Regenerative-dose （SAR） Protocol and Radiocarbon ^14C dating, the deposit ages of three-grade terraces were obtained, which are 57.5, 12.8 and 5.7 kaBP, respectively. The features and ages of terraces reveal that the incision rate of the stream accelerated at the beginning of the Holocene. The incision rate changed suddenly at 12.8 KaBP, from 0.43±0.07 mm/a to 1.59±0.55 mm/a. This implicates that uplift of the Kunlun Mountains is intensive at the first onset of the Holocene, corresponding to the obvious change of slip-rate on the AItyn Tagh Fault. But its uplift rate is much lower than that of the latter, which suggests that growth of the northern margin of the Tibetan Plateau is stronger than its interior.     

一类非线性控制系统的稳定干扰解耦

讨论了一类SISO非线性系统的干扰解耦问题,给出了非线性系统关于干扰的相对阶,通过静态状态反馈实现系统干扰的解耦可解条件以及系统稳定控制,最后通过仿真算例验证了该方法的有效性。     

张力控制器在热连轧机架间的应用

介绍了连轧张力状态方程、西门子张力计算模型、新日铁张力计算模型的计算公式,通过对渐近收敛状态观测器设计、张力动态互不相关控制(解耦控制)设计的叙述,解释了利用渐近收敛状态观测器提供的状态量,研究了张力增量的动态互不相关控制的内容,最后对各项技术指标、项目研究结论及其原理进行了分析。     

西藏亚勒-雄勒断裂带侵入岩体地球化学特征及构造成因

亚勒—雄勒断裂带是冈底斯板块与羌塘板块的分界断裂带 ,是班公湖—怒江断裂带中段的组成部分。对断裂带侵入岩岩体的岩石类型、岩石化学特征、岩石地球化学特征的研究表明 ,侵入岩石主要为闪长岩、石英闪长岩、角闪石闪长岩和花岗岩 ,属钙碱性岩石系列 ,具“Ⅰ”型花岗岩特征。其形成是由于在冈底斯板块与羌塘板块碰撞过程中 ,地壳物质发生熔融而沿断裂带侵入所致 ,为燕山晚期产物