商品混凝土降低成本的技术途径

商品混凝土目前价格偏高 ,用户不情愿接受 ,影响了它的推广应用。针对这一问题 ,本文提出了用“活化填料”、“活化水泥”配制高性能商品混凝土的技术路线并分析了其技术经济效益     

气推式脱壳弹充排气规律研究与计算

气推式脱壳弹以其结构简单、脱壳干扰小、无自伤等优点而具有广泛应用前景.该文对其弹托气室与炮膛间的充、排气规律进行了分析研究,计算了某航炮用气推弹气室内温度、密度和压力沿内弹道段的变化,分析了气孔面积对气室膛口压力的影响,为进一步研究气推弹瞠外脱壳规律提供理论依据.     

粉煤灰和木钙双掺用于胶结充填的正交组合试验

通过粉煤灰和木钙双掺用于尾砂胶结充填的交组合试验，提示了双掺的作用机理，建立了试验指标的二次回归程，得出了双掺时粉煤灰和木钙的最佳掺量。     

滩坑水电站面板堆石坝筑坝新工艺

滩坑水电站筑坝施工防渗墙施工不留龙口,实施先闭气后截流的导截流施工方案,使工期提前1个多月。采用抛石挤淤工艺,实现了基坑深覆盖层坝基开挖快速施工。汛期适当提高坝体填筑高程,在坝面高差处设置超径石保护,坝面经多次过流冲刷少,同时大大减少了溢洪道备料开挖。坝内预埋水管,高压水泵直供坝面喷射洒水,洒水均匀且经济安全。利用液压挖掘机作导向地锚,推土机牵引进行斜坡碾压,不需专用设备,坡面碾压质量好,实现了高面板坝优质快速施工。     

Study on Numerical Simulation of Mold Filling and Solidification Processes under Pressure Conditions

The mold filling and solidification simulation for the high pressure die casting (HPDC) and low pressure die casting (LPDC) processes were studied.A mathematical model considering the turbulent flow and heat transfer phenomenon during the HPDC process has been established and paralled computation technique was used for the mold filling simulation of the process.The laminar flow characteristics of the LPDC process were studied and a simplified model for the mold filling process of wheel castings has been developed.For the solidification simulation under pressure conditions,the cyclic characteristics and the complicated boundary conditions were considered and techniques to improve the computational efficiency are discussed.A new criterion for predicting shrinkage porosity of Al alloy under low pressure condition has been developed in the solidification simulation process.     

视觉技术在YP19装封箱机中的设计与应用

介绍视觉技术在YP19装封箱机的装箱过程中的应用,简述视觉技术系统的基本组成、工作原理及软件设计。     

最长公共子序列算法在填空题评分程序中的应用

讨论最长公共子序列算法在填空题评分中的应用,并具体设计一种基于网络环境下,考试系统中的填空题题型的通用答案识别逻辑,在独立学院网络考试系统中操作可行。     

水工建筑物下伏采空区稳定性评价及治理措施研究 ——以彬长矿区输配水工程为例

位于煤矿采空区上的水工建筑物,存在采空引起的沉陷问题,沉陷使采空区上覆岩层的围岩失稳,使地表变形呈现裂缝、塌陷台阶等不同型式的地质灾害,导致建筑物受损,并影响其安全稳定性,使工程建筑物不能发挥其功能。为此需对采空区进行勘察研究,研究其垮落型式和垮落体体积,在此基础上采用概率积分法,对建筑物下伏采空区引发的地表变形进行计算预测,分析评价剩余变形量的稳定性,确定建筑物下伏采空区治理标准,研究采空区的治理范围、防治措施、施工方法,提出质量控制要求。通过垂直钻孔、全胶结法灌浆充填的方法对深层煤炭采空区进行治理,用钻孔检测等多种方法对治理后的采空区进行检测,其倾斜值、曲率值、水平变形值、水平移动值和下沉量均小于采空区场地变形允许值。说明对剩余空洞体灌注混凝土的治理方法达到了预期效果,可以为同类采空区治理工程提供借鉴经验。     

1960-2016年贵州喀斯特山区干旱时空动态分析

干旱是造成喀斯特地区损失最为严重的自然灾害之一。以我国西南喀斯特集中分布区域为研究区,基于研究区33个气象站1960-2016年的逐日降水数据,利用PA指数和Mann-Kendall检验方法分析了1960-2016年干旱时空分布特征。结果表明:研究区降雨量有减少趋势,PA指数呈减小趋势,干旱呈增强趋势,2011年PA均值最小;研究区各季干旱强度均呈上升趋势,且冬旱强度最强、发生干旱年份最多,秋旱次之,春旱和夏旱强度较弱、发生干旱的年份较少;年际干旱频次高发区集中于研究区南部、西北部及中东部地区;仅秋、冬季西部和东南部部分地区出现特旱且频次低,秋、冬季发生重旱、中旱和轻旱的频次高,春、夏季较低;春季干旱频次西高东低,夏季中部高,秋季南高北低,冬季西高东低;干旱与地形因子显著相关,重、特旱易发生在高陡地区。综上所述,研究区干旱有增强趋势且秋、冬季趋势较强,空间上呈现明显的季节性和区域性,且与地形因子显著相关。     

Comparison of soil moisture at different depths for drought monitoring based on improved soil moisture anomaly percentage index

To better understand the characteristics and mechanisms of droughts at different drought stages, this study selected the Xiangjiang River Basin in China as the study area, and evaluated soil moisture (SM) at different depths for drought monitoring, through SM data simulated with the variable infiltration capacity (VIC) model. To solve the problem of unreasonable drought/wetness classifications based on the soil moisture anomaly percentage index (SMAPI), an improved soil moisture anomaly percentage index (ISMAPI) was developed by introducing the Box–Cox transformation. The drought/wetness frequency generated by ISMAPI demonstrated preferable spatial comparability in comparison with those from SMAPI. The lag time of ISMAPI relative to the standardized precipitation evapotranspiration index was closely related to soil depth, and was characterized by a fast response in shallow soil layers and a relatively slow response in deep soil layers. SM in shallow soil layers provided a measure for monitoring short-term droughts, whereas SM in deep soil layers provided a better measure for long-term persistent drought events. Furthermore, the occurrence and mitigation time of drought events identified by SM in deep soil layers usually lagged behind that identified by SM in shallow soil layers. Compared with deep SM, SM in shallow soil layers responded faster to meteorological anomalies, thereby resulting in shorter periods of SM persistence in shallow soil layers than in deep soil layers. This can explain the differences of SM at different depths in drought monitoring.