Dynamic-based model for calculating the boulder impact force in debris flow

The boulder impact force in debris flow is generally calculated by static methods such as the cantilever beam models.However,these methods cannot describe the dynamic scenario of boulder collision on structures,so the inertia and damping effects of the structures are not involved causing an overestimation on the boulder impact force.In order to address this issue,a dynamic-based model for calculating the boulder impact force of a debris flow was proposed in this study,and the dynamic characteristics of a cantilever beam with multiple degrees of freedom under boulder collision were investigated.By using the drop-weight method to simulate boulders within debris flow,seven experiments of drop-weight impacting the cantilever beam were used to calibrate the error of the dynamicbased model.Results indicate that the dynamic-based model is able to reconstruct the impact force history on the cantilever beam during impact time and the error of dynamic-based model is 15.3%in calculating boulder impact force,significantly outperforming the cantilever beam model’s error of 285%.Therefore,the dynamic-based model can overcome the drawbacks of the static-based models and provide a more reliable theoretical foundation for the engineering design of debris flow control structures.

Boulder-induced form roughness and skin shear stresses in a gravel-bed stream

Boulder spacing in mountain rivers and near-wake flow zones within the boulder array is very useful for fish habitat and growth of aquatic organisms.The present study aims to investigate how the boulder array and spacing influence the near-bed flow structures in a gravel-bed stream.Boulders are staggered over a gravel-bed stream with three different inter-boulder spacing namely(a)large(b)medium and(c)small spacing.An acoustic Doppler velocimeter was used for flow measurements in a rectangular channel and the results were compared with those acquired from numerical simulation.The time-averaged velocity profiles at the near-wake flow zones of boulders experience maximum flow retardation which is an outcome of the boulder-induced form roughness.The ratio of velocity differences associated to form and skin roughness and its positive magnitude reveals the dominance of form roughness closest to the boulders.Form roughness computed is 1.75 to 2 times higher than the skin roughness at the near-wake flow region.In particular,the collective immobile boulders placed at different inter-boulder spacings developed high and low bed shear stresses closest to the boulders.The low bed shear stresses characterised by a secondary peak developed at the trough location of the boulders is attributed to the skin shear stress.Further,the spatial averaging of time-averaged flow quantities gives additional impetus to present an improved illustration of fluid shear stresses.The formation of form-induced shear stress is estimated to be 17%to 23%of doubleaveraged Reynolds shear stress and partially compensates for the damping of time-averaged Reynolds shear stress in the interfacial sub-layer.The quadrant analysis of spatial velocity fluctuations depicts that the form-induced shear stresses are dominant in the interfacial sub-layer and have no significance above the gravel-bed surface.

Typhoon vs. cold wave: a comparative assessment of geomorphic response and boulder displacement using RFID technology

Extreme storm events in coastal zones play significant roles in shaping the morphology of boulder beaches.However,boulder displacement and the geomorphological evolution of boulder beaches driven by different extreme storm events,especially typhoon events,remain poorly understood.Thus,boulder displacement and the geomorphic response on a boulder beach in Fujian,southeastern China,were explored before,during and after a cold wave event(Dec.1–7,2020)and before and after Typhoon In-Fa(Jul.19–27,2021),a large tropical storm.This was achieved by tracking 42 tagged boulders distributed in the intertidal and supratidal zones using Radio Frequency Identification(RFID)and topographic surveys using real-time kinematic techniques,respectively.The results showed obvious disparities in boulder displacement in different geomorphic zones due to cold wave and typhoon events that were mainly characterized by migration magnitude,range,direction,and mode of transport.The typhoon event led to rapid and substantial changes in the overall morphology of the boulder beach,while the cold wave event impacted the intertidal morphology of the boulder beach to only a small extent.The surrounding structure of boulders,beach slope and beach elevation had a combined dominant effect on boulder displacement under the same extreme event.Hydrodynamic factors(effective wave energy fluxes,incident wave direction,storm surge and water level)had dominant effects on boulder displacement during different extreme events.In terms of a single event,the magnitude of the boulder displacement driven by the typhoon was much greater than that driven by the cold wave.However,considering the frequency and duration of cold waves in winter,the impact of multiple consecutive cold waves on the geomorphology of the boulder beach cannot be ignored in this study area.Alternating and repeated interactions between these two processes constitute the complete geomorphic evolution of the boulder beach.This study contributes to improved predictions of the morphodynamic response of boulder beaches to future storms,especially large tropical storms,and facilitates better coastal management.

中凯矿业大直径深孔爆破落矿装药结构优化研究

装药结构对厚大矿体大直径深孔爆破落矿效果具有重要影响。中凯矿业帮中矿区现行装药结构(空气间隔长度比例24.2%)存在爆破后冲破坏作用严重的问题,造成后一排炮孔堵塞、坍塌甚至报废,严重影响生产效率;而盲目增大空气间隔长度比例则存在爆破大块率增加的风险。以矿山实际的炸药和岩石参数为基础,采用数值模拟软件LSDYNA开展大直径深孔爆破落矿装药结构优化研究。选择常用空气间隔器作为间隔材料,以空气间隔长度比例为研究对象设计了12种装药结构方案进行数值模拟,得到了装药结构与爆破后冲作用、大块率、自由面质点振动峰值速度以及峰值有效应力等评价指标之间的关系。结果表明:自由面质点振动峰值速度以及峰值有效应力随空气间隔长度比例增加逐渐下降;当空气间隔长度比例小于等于30.5%时后冲作用明显,后排炮孔可能出现塌孔现象,当空气间隔长度比例大于等于45.3%时,存在大块率增加的风险,最优装药结构的空气间隔长度比例为44.2%。现场深孔爆破落矿试验表明,优化的装药结构爆破后大块率为7.1%且爆破后冲作用得到有效控制。

泥石流中球形巨石运动规律模型试验研究

该研究通过室外水槽模型试验,模拟了不同直径巨石与不同密度泥石流完全固液耦合作用下的运动状态,分析了泥石流沟内巨石在泥石流中的运动模式、运动的影响因素及其在泥石流中的受力情况,并探讨了泥石流密度与巨石粒径对其运动速度的影响。研究结果表明:巨石在运动过程中可能出现滚动、跳跃与滑动等运动模式,巨石出现的运动模式同泥石流的密度以及巨石粒径有关;巨石的直径越大,运动速度越小,它在泥石流中的运动模式越简单,越倾向于发生滚动运动,在泥石流流体中的跟随性越好,速度比n越容易趋近于1;巨石粒径对巨石运动速度的影响大于泥石流密度对它的影响。

Evolution of tectonic landscapes and deformation in the southeast Kumaun and western Nepal Himalaya

The area of the present investigation’s expanse constitutes the southernmost extent of the southeast Kumaun Himalaya and western Nepal Himalaya.Multidisciplinary approaches have been employed to understand the landforms associated with tectonic deformation,through detailed field investigation supplemented by the geodetic,chronological,and morphometric database.The morphogenic expressions of the Main Boundary Thrust(MBT)are reflected in the form of~25 km long E-W trending north dipping fault scarp.The deformation along the strike length of the Himalayan Frontal Thrust(HFT)is noticed in the form of uplifted and incised fill terraces,and strath terraces.The deformation within the fluvial sequences in the study area can be visualized in the form of sheared boulders and pebbles,tilted and faulted terrace deposits.Furthermore,the chronological data of fluvial landforms in the study area suggests two major phases of tectonic deformations that have occurred around 58.7±10.8 ka and 3.88±0.4 ka.The chronology of late-Quaternary landforms advocates that the initial stage of aggradations in the Himalayan foothills commenced around 75.1±0.58 ka.The aggradational landforms resulted from the diverse depositional regime as evident from the nature of the sediment sequences from clasts dominated to thick mud sequences.The rate of deformation in the southeastern Kumaun and western Nepal Himalaya is±7 mm/yr,as per the data obtained from the Persistent Scatterer Interferometric Synthetic Aperture Radar(PSInSAR).The landform deformation pattern,phase of incision and aggradation,frequent occurrence of landslides,and recent past earthquake activity within the wide zone of the HFT,the MBT,and Ramgarh Thrust suggests that the southernmost front of the Kumaun Himalaya is active and has potential for future geohazard.The foothill zone of Himalayan towns are actively growing in terms of population and infrastructural development.Therefore,such intradisciplinary studies for tectonically active regions are needed for future infrastructural development.

岩溶区域内地下连续墙施工中问题探讨

地下连续墙等基坑支护施工时会遇到各种各样的复杂地层,岩溶即其中之一。岩溶地质条件对于地下连续墙施工极为不利。基于实际施工经验,对成槽施工前溶洞勘察、成槽过程中岩溶问题处理进行详细讨论。讨论内容包括:溶洞中存在漂石、斜岩情况的处理以及溶洞导致的塌方和路面下沉等问题的处理,并基于实际经验给出部分岩溶区域地下连续墙施工建议。

软硬交替地层超深竖井受力特性及合理分层开挖厚度探讨

某检修排水井尺寸规模大,开挖深度深,所处地层条件复杂,具软硬交替特征。为确保竖井深基坑开挖稳定性,提高施工效率,利用三维数值模拟软件FLAC3D对该超深竖井基坑开挖施工全过程进行仿真模拟,分析5种不同分层开挖厚度情况下超深竖井结构受力和变形特性。研究表明:1)地连墙的最大环向应力和最大水平位移均随分层开挖厚度的增加而增加,在软岩地层范围内出现应力和变形突增,在硬岩地层范围内出现应力和变形骤减;2)以无内衬开挖下地连墙最大环向应力和最大水平位移为参考标准,单层开挖厚度范围为3~4 m对地连墙位移具有很好的约束效果,建议实际工程中土层开挖及软岩开挖时采用3 m分层厚度,硬岩部分地层开挖时采用4 m分层厚度。

珠海某高陡斜坡孤石稳定性分析评价

本文依托珠海市第二中学后山孤石(典型危岩体)应急工程勘查项目,通过野外调查和模拟孤石失稳可能滚落的距离、弹跳高度,研究孤石发育规模特征,对孤石的稳定性进行了定性评价和定量分析,对孤石状态变化趋势及危害性进行了预测,并提出防治建议。

滨海城市地质结构电阻率法三维模拟与应用

在我国滨海城市地下工程建设中,精准定位断层、孤石及其他不良地质体是亟待解决的技术问题之一。基于滨海城市地质特点,针对高密度电阻率法开展了三维数值模拟研究,获得了覆盖层电性和厚度对高密度电阻率探测的影响结果,以及探测目标体大小和埋深发生变化时的直流电场特征。研究结果表明:覆盖层与探测目标的电阻率的差异大小是决定覆盖层影响的主要因素,对于低阻断层破碎带,覆盖层电阻率越高,破碎带的响应越突出。在中高阻覆盖条件下,孤石埋深越浅越容易获得揭露,尺寸越大其高阻特征越突出。在青岛市地铁5号线勘查中,高密度电阻率法在断裂破碎带和孤石探测中显示出关键作用,验证了方法的应用效果。研究成果可为滨海城市工程勘查方法选择和工作参数确定提供依据。

浅谈城市矿山法隧道穿越圆砾土层加固技术

某城际铁路滨市区间隧道采用矿山法施工,较长地段穿越圆砾土层。为确保建构筑物的安全,采用地表高压旋喷加固,洞内超前周边加固注浆,洞内径向注浆及管棚套小导管的方式,对洞内外综合加固,起到了良好的止水效果。通过施工效果检验,洞内、地表沉降变形控制在允许范围以内,保证了隧道施工和周边建构筑的安全。

基于声波频谱特征的土体障碍物超声探测分析

为了探究超声波法对土体中障碍物的探测效果,以上海市某地区的黏性土为介质设计了室内试验,并通过改变土的含水率和超声探测距离来研究不同因素对超声探测效果的影响。通过傅里叶变换对试验结果进行频谱特征分析,分别从含水率、探测距离、障碍物三个方面分析不同影响因素下接收信号的频谱变化规律。研究结果表明:随着含水率的增大,接收信号的频谱畸变程度减小,曲线上的突变点减少;随着探测距离的增大,接收信号的频谱畸变程度增大,曲线上的突变点增多;在含水率较低的情况下,障碍物的存在对接收信号频谱的影响忽略不计,在含水率较高的情况下,障碍物的存在会导致接收信号的频谱畸变程度增大,可以从频谱上进行识别。

海域花岗岩发育区地震反射精细地质构造调查

广东近海海域位于太平洋板块与大陆板块交界处,地质活动活跃,地质结构复杂。在花岗岩分布区,基岩不均匀风化形成风化基岩凹槽、隆起和孤石等,基岩面起伏较大。单一钻探方法难以反映隧道沿线地质结构的连续变化。本文采用高频小炮距水域地震反射方法,查明隧道沿线详细地质条件,总结各种地质体的地震反射特征,研究断裂走向及活动性。在小炮间距地震剖面中,基岩面表现为反射同相轴起伏变化,基岩隆起对应同相轴上隆,基岩凹槽对应同相轴下凹;断裂表现为同相轴缺失、突变、错断;抛石发育区与孤石(群)形成绕射波。本文利用多条地震反射剖面构建三维地质模型,全面展示隧道沿线复杂地质结构,划定强风化花岗岩区。对比研究发现地震反射解释结论与钻探揭示情况吻合较好,为隧道工程设计和施工提供了可靠的地质资料。

大粒径富水卵石、漂石土地层大直径土压盾构掘进关键技术

为解决大直径土压盾构在大粒径富水卵石、漂石土地层条件下刀盘刀具磨损严重、刀盘被卡、地表塌陷、渣土喷涌等工程难题,结合都四山地轨道交通项目DSZQ-1标永丰站—蒲阳站区间盾构隧道工程的施工情况,从盾构选型设计、超前地质预警处理、掘进参数选择、渣土改良、螺机防喷涌等方面进行研究,总结出都江堰地区大粒径富水卵石、漂石土地层大直径土压盾构掘进关键技术,为后续工程在此类地层施工提供了借鉴依据。

边坡花岗岩风化孤石工程危险性评价方法研究

对边坡花岗岩风化孤石工程危险性预测时尚无规范依据和行之有效的方法。影响边坡花岗岩风化孤石稳定性的因素较多且不确定性较强,引入层次分析法,建立危险性评价层次结构模型,根据工程实践经验和反馈给出影响因素重要程度评判矩阵,从而得到影响因素重要程度权重矩阵,根据各影响因素定性评分得到危险性评价结论,且具有半定性半定量的特点。通过工程对比,有较好的一致性。

缙云老城区条石建筑文化保护传承与创新发展

从缙云老城区条石建筑的现状入手,梳理了缙云条石建筑的发展历程,经实地调研总结出其数量多和类型丰富的特点。通过对建筑本身的历史、科学、艺术和情感价值的解析,总结出缙云老城区条石建筑保护与再利用的策略:整合资源,营造特色文化场馆;构建体系,打造主题文化街区;打通生态,开辟文化旅游线路。以期让这些条石建筑生命得到延续,老城区的历史文化得到传承。

弱胶结宽级配卵漂石工程地质特性及边坡稳定性研究

青藏高原山区河流阶地发育,区域内卵漂石具有弱胶结、宽级配、超大粒径颗粒含量较多等特点,工程地质特性及边坡稳定性研究难度大。采用现场原位试验、室内试验和地质调查测绘等方法,初步查明西藏扎拉水电站工程区卵漂石颗粒级配及抗剪强度。通过近景测量摄影、图像处理技术与常规颗粒分析试验相结合可确定颗粒级配,基于实测边坡地形和调查稳定坡角,结合稳定性反演计算可获得抗剪强度参数。结果表明:天然和饱水条件下卵漂石的内摩擦角差别不大,但饱水条件黏聚力仅为天然条件的25%~40%,由此对正常蓄水位以下、以上的库坝区边坡分别采取不同的支护措施,确保了处理方案的安全性与经济性。研究结果可为库坝区卵漂石边坡稳定性计算评价及处理方案设计提供地质依据。

西藏扎拉水电站主要工程地质问题研究

西藏扎拉水电站地处青藏高原东构造结,地质条件复杂,为分析其工程建设和运营面临的地质风险,通过工程地质勘察,查明了工程区基本地质条件,论证了主要工程地质问题及影响。结果表明,扎拉水电站主要工程地质问题为:(1)水库坍岸、倾倒岸坡稳定及固体径流问题;(2)坝址坝肩倾倒边坡、近坝卵漂石岸坡、坝基抗滑稳定问题及坝基防渗问题;(3)引水发电系统中引水隧洞受闹中活动断裂影响、引水隧洞及调压室围岩稳定问题、厂房后倾倒边坡稳定问题等。针对以上问题,提出了相应处理措施。研究成果可为工程建设提供科技支撑。

高流速大粒径漂卵石复杂条件下非通航河道疏浚施工技术研究

水电开发项目通过拓挖水电站下游河道以增加水头、提高装机容量可以取得良好的经济效益。然而,受河道水文气象、地质条件等现场复杂条件的影响,部分电站下游河道不具备拓挖条件。阐述了大渡河沙坪一级水电站下游河道治理工程,针对高流速、大粒径漂卵石复杂条件下非通航河道疏浚施工技术进行的研究,提出了复杂条件下河道疏浚技术难题的解决思路及方法,所取得的经验可为类似工程疏浚施工提供参考。

Evaluation and optimization of blasting approaches to reducing oversize boulders and toes in open-pit mine

A new blasting approach of combined blastholes with different diameters is proposed to solve the problems of oversize boulders and rock toes in open-pit mine. A non-ideal detonation model and a statistical damage constitutive model are implemented in dynamic finite element analysis to investigate the formation mechanism of oversize boulders and toes. The damage distribution and evolution process of rock blasting fragmentation is simulated, and the scheme is further optimized. Numerical analysis results showed that pocket charges and satellite blastholes can only improve bench top fragmentation, but they cannot reduce the oversize in the middle and bottom of bench as well as the toe problem. The new blasting approach of combined blastholes with different diameters can effectively reduce the oversize boulders and toes as well as the production costs.