Heat transfer and temperature evolution in underground mininginduced overburden fracture and ground fissures: Optimal time window of UAV infrared monitoring

Heat transfer and temperature evolution in overburden fracture and ground fissures are one of the essential topics for the identification of ground fissures via unmanned aerial vehicle(UAV) infrared imager. In this study, discrete element software UDEC was employed to investigate the overburden fracture field under different mining conditions. Multiphysics software COMSOL were employed to investigate heat transfer and temperature evolution of overburden fracture and ground fissures under the influence of mining condition, fissure depth, fissure width, and month alternation. The UAV infrared field measurements also provided a calibration for numerical simulation. The results showed that for ground fissures connected to underground goaf(Fissure Ⅰ), the temperature difference increased with larger mining height and shallow buried depth. In addition, Fissure Ⅰ located in the boundary of the goaf have a greater temperature difference and is easier to be identified than fissures located above the mining goaf. For ground fissures having no connection to underground goaf(Fissure Ⅱ), the heat transfer is affected by the internal resistance of the overlying strata fracture when the depth of Fissure Ⅱ is greater than10 m, the temperature of Fissure Ⅱ gradually equals to the ground temperature as the fissures’ depth increases, and the fissures are difficult to be identified. The identification effect is most obvious for fissures larger than 16 cm under the same depth. In spring and summer, UAV infrared identification of mining fissures should be carried out during nighttime. This study provides the basis for the optimal time and season for the UAV infrared identification of different types of mining ground fissures.

Determination of minimum overburden depth for underwater shield tunnel in sands:Comparison between circular and rectangular tunnels

With the development of global urbanization,the utilization of underground space is more critical and attractive for civil purposes.Various shapes of shield tunnels have been gradually proposed to cope with different geological conditions and service purposes of underground structures.Generally,reducing the burial depth of shield tunnel is conducive to construction and cost saving.However,extremely small overburden depth cannot provide sufficient uplift resistance to maintain the stability and serviceability of the tunnel.To this end,this paper firstly reviewed the status of deriving the minimum sand over-burden depth of circular shield tunnel using mechanical equilibrium(ME)method.It revealed that the estimated depth is rather conservative.Then,the uplift resistance mechanism of both circular and rectangular tunnels was deduced theoretically and verified with the model tests.The theoretical uplift resistance is consistent with the experimental values,indicating the feasibility of the proposed equations.Furthermore,the determination of the minimum soil overburden depth of rectangular shield tunnel under various working conditions was presented through integrated ME method,which can provide more reasonable estimations of suggested tunnel burial depth for practical construction.Additionally,optimizations were made for calculating the uplift resistance,and the soil thickness providing uplift resistance is suggested to be adjusted according to the testing results.The results can provide reference for the design and construction of various shapes of shield tunnels in urban underground space exploitation.

Kinetics of solid-state reduction of chromite overburden

The demand for alternative low-grade iron ores is on the rise due to the rapid depletion of high-grade natural iron ore resources and the increased need for steel usage in daily life.However,the use of low-grade iron ores is a constant clinical task for industry metallurgists.Direct smelting of low-grade ores consumes a substantial amount of energy due to the large volume of slag generated.This condition can be avoided by direct reduction followed by magnetic separation(to separate the high amount of gangue or refractory and metal parts)and smelting.Chromite overburden(COB)is a mine waste generated in chromite ore processing,and it mainly consists of iron,chromium,and nickel(<1wt%).In the present work,the isothermal and non-isothermal kinetics of the solid-state reduction of self-reduced pellets prepared using low-grade iron ore(COB)were thoroughly investigated via thermal analysis.The results showed that the reduction of pellets followed a firstorder autocatalytic reaction control mechanism in the temperature range of 900-1100℃.The autocatalytic nature of the reduction reaction was due to the presence of nickel in the COB.The apparent activation energy obtained from the kinetics results showed that the solid-state reactions between COB and carbon were the rate-determining step in iron oxide reduction.

Experimental study on the interrelation of multiple mechanical parameters in overburden rock caving process during coal mining in longwall panel

In order to comprehend the dynamic disaster mechanism induced by overburden rock caving during the advancement of a coal mining face, a physical simulation model is constructed basing on the geological condition of the 21221 mining face at Qianqiu coal mine in Henan Province, China. This study established, a comprehensive monitoring system to investigate the interrelations and evolutionary characteristics among multiple mechanical parameters, including mining-induced stress, displacement, temperature, and acoustic emission events during overburden rock caving. It is suggested that, despite the uniformity of the overburden rock caving interval, the main characteristic of overburden rock lies in its uneven caving strength. The mining-induced stress exhibits a reasonable interrelation with the displacement, temperature, and acoustic emission events of the rock strata. With the advancement of the coal seam, the mining-induced stress undergoes four successive stages: gentle stability, gradual accumulation, high-level mutation, and a return to stability. The variations in other mechanical parameters does not synchronize with the signifcant changes in mining-induced stress. Before the collapse of overburden rock occurs, rock strata temperature increment decreases and the acoustic emission ringing counts surges with the increase of rock strata displacement and mining-induced stress. Therefore, the collaborative characteristics of mining-induced stress, displacement, temperature, and acoustic emission ringing counts can be identifed as the precursor information or overburden rock caving. These results are in good consistent with on-site situation in the coal mine.

3D forward modeling and response characteristics of low-resistivity overburden of the CFS-PML absorbing boundary for ground-well transient electromagnetic method

This study used the stable and convergent Dufort-Frankel method to differentially discretize the diffusion equation of the ground-well transient electromagnetic secondary field.The absorption boundary condition of complex frequency-shifted perfectly matched layer(CFS-PML)was used for truncation so that the low-frequency electromagnetic wave can be better absorbed at the model boundary.A typical three-dimensional(3D)homogeneous half-space model was established and a low-resistivity cube model was analyzed under the half-space condition.The response patterns and drivers of the low-resistivity cube model were discussed under the influence of a low-resistivity overburden.The absorption boundary conditions of CFS-PML significantly affected the low-frequency electromagnetic waves.For a low-resistivity cube around the borehole,its response curve exhibited a single-peak,and the extreme point of the curve corresponded to the center of the low-resistivity body.When the low-resistivity cube was directly below the borehole,the response curve showed three extreme values(two high and one low),with the low corresponding to the center of the low-resistivity body.The total field response of the low-resistivity overburden was stronger than that of the uniform half-space model due to the low-resistivity shielding effect of electromagnetic waves.When the receiving-transmitting distance gradually increased,the effect of the low-resistivity overburden was gradually weakened,and the response of the low-resistivity cube was strengthened.It was affected by the ratio of the overburden resistivity to the resistivity of the low-resistivity body.

Geochemical and mineralogical evaluations of coal,shale,and mine waste overburden from Makum coalfield of the Northeast India

The Cenozoic-age Makum coal from northeastern India offers numerous research opportunities because of its diverse geochemical and geological characteristics.Due to its high sulfur content,the coal has been found to be less useful for industrial purposes.It can,however,serve as a hub for ongoing research on coal-based derivative products.The aim of this research work is to investigate the mineralogical and geochemical compositions of the coal,mine overburden(MOB)and shale samples taken from the Makum coal field and also on establishing a mutual relationship between them.To characterize the geochemical controlling factors of the Makum coal field,the study employs coal petrography,FTIR,mineralogical,and geochemical analysis.According to X-ray diffraction analysis,the major minerals like quartz,kaolinite,haematite,illite,pyrite,and calcite are present in coal and MOB.Pyrite is observed by SEM-EDS analysis as cubic-shaped particles that are smaller than a fewμm in size.The presence of sulfide minerals represents a phase of pyrite mineralization.The petrography study was used to better understand the environment that existed during the formation of the plant material,which aids us in determining the quantity of detrital mineral sediment contained in the coal.According to the ICP-MS analysis,the samples indicate significant levels of rare earth elements including yttrium.The present study reveals higher concentrations of poten-tial hazardous elements in the coal samples,with V,Cr,Ni,Cu,and Zn content in coal being considerably enriched compared to world-average concentrations.The correlation analysis reveals that the potential hazardous elements like Co,Ni,As,and Cu are associated with pyrite as they have strong affinity towards pyrite.Thus,numerous minerals and rare earth elements(REEs)exist,opening up a fresh avenue for more research in the area.This study also assists researchers in understanding the significance of Makum coal and provides numerous ideas for coal characterization.

深厚覆盖层上土石坝防渗墙损伤开裂精细化分析及防渗功能评价

混凝土防渗墙是覆盖层上土石坝坝基的关键防渗结构,由于防渗墙与覆盖层的刚度和尺度差异巨大,通常的数值分析方法难以保证精度,且现有基于强度的安全评价方法,无法适应防渗墙作为防渗结构而非承载结构的功能评价要求。本文提出了比例边界元-有限元耦合跨尺度离散、塑性损伤模型和内聚力模型分离描述压损伤和受拉开裂、破损后防渗功能目标评价的精细化分析方法,实现了深厚覆盖层上土石坝防渗墙的性态演化评价。研究结果表明:超深覆盖层上悬挂式防渗墙在两岸底部因近似垂直于岸坡的高压应力发生压损伤,类“外伸梁”的面内弯曲变形使靠近防渗墙两岸的顶部和底部区域产生坝轴向高拉应力导致槽段间出现竖向裂缝;在防渗墙两岸的上游侧局部设置辅助防渗措施,可有效降低防渗墙破损后的渗流量。本文方法揭示了混凝土防渗墙的损伤开裂模式,定位了防渗墙薄弱区域,评价了防渗墙损伤开裂对防渗功能的影响,量化防渗措施效果,实现了防渗墙从传统承载能力评价到功能性态评价的跨越,可为深厚覆盖层上土石坝防渗墙的安全评价和设计优化提供理论和技术支持。

厚煤层大采高综放工作面覆岩断裂演化规律研究

大采高综放开采易形成强烈的矿压显现,上覆岩层的断裂演化规律对工作面安全生产至关重要。以羊场湾煤矿160206工作面为工程背景,运用相似模拟试验、数值模拟和理论分析的综合研究方法,对大采高综放工作面覆岩的断裂过程与覆岩运移规律进行系统研究。研究表明:导水裂隙带内岩层随工作面推进表现为“台阶下沉”,同层岩层下沉趋势沿走向表现为“急剧下降—稳定(最大值)—快速上升—稳定(最小值)”。工作面覆岩运动场由两区分布(加速下沉区、缓慢下沉区)演化为三区分布(加速下沉区、缓慢下沉区、稳定区)。对离层演化与地表下沉规律进行了定量描述,运用理论计算表达式深入地剖析了地表的动态下沉机理及其相关因素。结合相似模拟与数值模拟的试验结果,提出了覆岩断裂演化的形态变化特征:覆岩断裂形态由“单等腰梯形”演化为“双等腰梯形”,表土层影响区由“矩形”演化为“倒梯形”。分析了覆岩中垮落区、离层区、压实区、裂隙富集区的动态演化过程:垮落区逐渐增大至一定程度,高度小幅度降低并趋于稳定,离层区由下至上逐渐发育并随工作面向前移动,离层区逐渐闭合形成压实区,且压实区逐渐增大并最终保持稳定,裂隙富集区位于采空区前后端部并随工作面向前移动。

小断层影响下的采空区瓦斯运移规律研究

在煤矿开采过程中,小断层会导致采空区瓦斯聚集形成瓦斯富集区,对生产安全具有很大威胁,因此有必要研究小断层影响下的采空区瓦斯运移规律。通过UDEC数值模拟采空区上覆岩层破坏过程,从而计算小断层影响下采空区上覆岩层的空隙率,并利用FLUENT软件数值模拟开采过程中考虑小断层影响的采空区瓦斯运移规律。研究表明:①工作面距离小断层20 m远处,小断层从顶部首先出现滑移现象,采空区上覆岩层的位移开始受到断层的影响;工作面到达断层时,由于断层滑移,上盘岩体在断层面滑移产生回转现象,支撑着采空区岩层,覆岩垮落位移量出现大幅度减小,并且岩层垮落出现滞后现象;小断层的影响范围有限,工作面过小断层60 m之后,采空区上覆岩层位移规律逐渐恢复正常。②通过分析含小断层采空区上覆岩层位移特征,得到了采空区上覆岩层位移及其拟合公式,计算得到了三维空隙率分布规律:垮落带范围内,覆岩空隙率在4个隅角位置最大,并且断层靠近进回风巷的位置也出现了空隙率增高;裂隙带范围内,除断层靠近进回风巷的位置空隙率较大,其他位置空隙率相对较低且变化不明显。③获得了小断层影响下的采空区瓦斯运移规律:在工作面距离断层50 m远处,采空区瓦斯运移几乎不受断层的影响;在工作面推进至断层时,瓦斯沿着断层及其附近的高空隙率覆岩产生的优势逃逸通道向采空区深部运移,同时上盘的瓦斯也向深部转移导致大量瓦斯积聚在断层下盘,可能导致瓦斯随漏风流入工作面及回风巷;在工作面过断层50 m时,采空区瓦斯继续向上隅角附近转移;工作面过断层100 m时,采空区上覆岩层瓦斯运移出现回转现象,上隅角和下盘垮落带瓦斯体积分数高。

深部条带老采空区覆岩破坏多参量监测研究

针对深部条带老采空区覆岩移动变形问题,确定了裂隙发育、拉压应变、岩层物性等主要参量指标,采用钻孔电视法、分布式光纤感测法、井间电法CT、微震法构建了采空区覆岩“点-线-面-体”多参量监测模式;运用该监测模式对工程实例进行实测分析,获取了采空区覆岩全方位、多层次的移动破坏特征,得出覆岩裂隙多集中在465 m以下,少量空洞位于垮落带及煤柱上方靠近采空区侧,煤柱塑性区范围约8 m的结论,综合判定采空区覆岩结构可在长时间内保持相对稳定。结果表明:“点-线-面-体”多参量监测模式在内容上能够有效涵盖条带采空区覆岩移动变形的各参量指标,时空上可实现点(静态)、线(动态)、面(静态)、体(动态)相互结合的全过程监测,监测结果间能相互验证,可满足深部条带采空区覆岩移动变形监测要求。

深覆土梯形拱明洞静力特性及卸荷效果

为研究深覆土条件下梯形拱结构–填土相互作用对周围土压力的影响机制和卸荷机理,明确梯形拱明洞相较于传统矩形明洞的优势,采用室内模型试验和数值模拟相结合的方法,对深覆土梯形拱明洞静力特性及卸荷效果进行分析。结果表明:无减载时,梯形拱明洞两侧回填土沉降大于上方回填土沉降,两侧回填土土压力向明洞上方转移,土压力随着填土高度的增大而增大,基本呈线性变化趋势;减载时,明洞上方回填土沉降大于两侧回填土沉降,回填土内部产生土拱效应,明洞上方回填土土压力向两侧转移,铺设减载层不会改变深覆土明洞结构受力分布,但会极大地减小其内力及变形,并提高结构安全系数;减载后,梯形拱明洞的最大轴力、最大正弯矩和最大负弯矩分别减少17.5%、34.1%、29.9%,最大变形减小32.9%。矩形和梯形两种截面形式下明洞的最大轴力均出现在中隔墙底部,最大正弯矩、最小安全系数和最大变形均出现在顶板中央位置;铺设减载层后两种截面形式拱明洞最小安全系数分别增大42.6%和100.0%,梯形拱明洞安全系数提高的比例更大,效果更显著。该研究可为深覆土梯形拱明洞结构的设计和施工提供理论指导和技术支持。

超深覆盖层上面板坝防渗墙连接板接缝变形机制及优化分析

针对超深软弱覆盖层上的面板坝工程止水缝安全问题,从变形和应力2个方面开展优化研究,揭示了防渗墙连接板趾板面板防渗体系的变形模式,定位了薄弱位置,提出了优化方案,并量化了工程应用效果.结果表明,防渗墙与趾板间沉降差集中在防渗墙与连接板之间的止水缝处,设置多块连接板无法起到逐步过渡沉降差的作用.防渗墙下游侧设置侧向支撑、制作倾斜形止水缝、趾板下设支撑墙均可减小防渗墙连接板间止水缝沉陷变形.相比垂直止水缝和多块连接板的传统方案,所提的防渗墙顶部拓宽连接板倾斜形止水缝以及防渗墙顶部拓宽倾斜形止水缝趾板下设支撑墙的深厚覆盖层上面板坝防渗体系综合优化方案可使防渗墙与连接板之间止水缝沉陷变形分别减小41.5%和53.8%.

结构瞬变影响下采场煤岩静态力学响应的阶变规律

为了明确采场煤岩力学响应的演变规律,以宽沟煤矿W1143长壁综采工作面为工程背景,采用物理相似模拟实验和数值计算相结合的方法,在明确来压前、后覆岩空间结构瞬变特征的基础之上,建立了一种实现坚硬岩层瞬时破断的数值模拟前处理方法,研究了结构瞬变影响下采场煤岩静态力学响应的阶变规律。结果表明:覆岩空间结构是由破裂面以外、采动影响范围以内不同岩性的岩层所组成的空间岩体结构,是其影响范围内的采场煤岩产生不同力学响应的内因。来压期间,由于坚硬岩层的破断具有瞬时性,导致覆岩空间结构发生瞬变,受此影响,采场煤岩的静态力学响应发生阶变,其本质上为一动力学过程。覆岩空间结构瞬变造成采场煤岩的应力场与位移场产生阶变,阶变集中于瞬变区域附近,距离瞬变区域越远,其阶变量越小。

巨厚覆岩矿震孕育破裂特征与应力触发机制

【目的】深部开采巨厚覆岩破断导致引起地表震感的矿震频发,已成为制约矿区高效生产的最严峻难题,亟待改变矿区巨厚覆岩矿震频度高、防控难现状。【方法】以内蒙古自治区鄂尔多斯呼吉尔特矿区某邻空综采工作面频发巨厚覆岩矿震为研究对象,应用厚板理论分析巨厚覆岩结构破断演化规律,提取矿震波形主成分并采用矩张量反演方法定量研究矿震震源破裂机制,基于张拉、压缩及混合破裂震源主应力作用方式修正应力反演模型,改进应力反演算法,分析矿震震源孕育破裂特征及应力场演化规律,定量解析矿震应力触发机制。【结果和结论】结果表明,巨厚覆岩破断运移为矿震孕育触发的动力、能量源;主成分分析方法可快速提取因采矿环境干扰波形的主成分,为矩张量求解提供优质反演数据;修正后应力反演算法能够满足采动诱发非剪切破裂震源应力反演需求,实现对典型张拉、压缩等非剪切破裂矿震震源应力场反演;工作面邻空回采期间,顶板逐层向上与侧向采空区联动破断,采空区影响使得孕震期间顶板活动性增强,巨厚覆岩断裂特征整体呈显著张拉状态;矿震孕育过程中主应力作用方位基本一致,应力形因子分别为0.66、0.71和0.30,覆岩应力分布由单轴挤压转变为挤压张拉状态,最大主应力单轴挤压作用导致巨厚覆岩瞬时断裂释放大量弹性能是诱发“2·6”和“10·30”矿震的主要原因,工作面邻更大范围采空区开采,最大、最小主应力挤压张拉协同作用将可能诱发更大能级矿震。研究结论可为矿区及周边因矿震问题限制高效生产的矿井从源头调控降载减震提供理论支撑。

水电工程深厚覆盖层地基防渗设计与潜蚀问题

我国西部一些水电站的坝址存在超深厚覆盖层,给工程的渗流控制和设计带来巨大的困难。垂直防渗墙是深厚覆盖层地基渗流控制最常用的措施。通过回顾泸定水电站深厚覆盖层悬挂式防渗墙地基异常渗漏治理的案例,指出对于西部河流中广泛存在的不稳定砂砾石地层,在关注渗流出口保护的同时,还应重视地基内部高流速和高水力梯度区域的潜蚀风险。为定量评价砂砾石地基内部潜蚀及其导致的后果,应开展深厚覆盖层内部稳定性评价准则、高上覆压力下砂砾石潜蚀试验技术、潜蚀数值模拟方法及潜蚀本构模型等关键技术问题的研究。

基于构造变形岩相带的覆盖区化探资料解释与找矿应用:以广西金秀镍钴多金属矿田为例

覆盖区化探资料复杂,解释难度大,亟须加强构造控矿要素方面的约束。不同类型覆盖区的构造形迹出露程度差别很大,因此需要从多个级别的构造体系中提取含矿构造变形岩相带的分布信息。本文提出基于地质力学构造体系阶段性演化特征判别覆盖区有利含矿构造走向,解译化探资料的成矿信息,以快速圈定找矿靶区的新思路。首先,从已知的地质、遥感和物探资料中解译出矿田的构造形迹和热液矿床的成矿信息;其次,依据成矿期的构造应力场特征确定主应力方向;第三,将张扭性和张性构造变形岩相带作为有利的含矿构造;最后,根据数据处理结果确定找矿异常区。将上述方法应用在广西金秀镍钴多金属矿田,确定了两个主要的含矿构造方向,即NWW—EW—NEE向断裂和NW—NNW向断裂,它们的形成时期不同,分别控制富砷化物型和富硫化物型的镍钴多金属矿脉。该方法和找矿思路可在覆盖区矿产资源勘查工作中进一步推广。

河流下综放工作面覆岩破坏特征和陷落柱防水煤柱留设研究

目的长平矿Ⅲ2317工作面在开切巷处揭露陷落柱,地表丹河流向与工作面推进方向一致,受采动影响,陷落柱内部水体及河水可能通过开采裂隙导入回采空间,从而造成工作面突水。针对以上问题,方法本文采用理论分析、数值模拟和现场观测等方法,对回采工作面覆岩“两带”高度、覆岩破坏特征和陷落柱煤柱留设宽度进行研究。结果结果表明:工作面顶板垮落带与导水裂隙带最大发育高度分别为18.38,93.85 m,河水对工作面不构成突水威胁;无煤柱开采时,陷落柱一侧顶板裂隙沿陷落柱胶结面向上高度发育;结合理论计算和数值模拟分析,确定煤柱宽度为35 m。工作面在留设35 m煤柱条件下安全完成回采,地表变形特征符合预期,最大下沉量达到4000 mm,回采过程中工作面未发生突水事故。结论研究结果可为类似条件下的煤层安全开采提供理论和经验支撑。

厚硬岩层结构调控低损开采方法及机理研究

为探究厚硬岩层采动结构对上覆岩层下沉破坏影响及新的低损开采方法,采用相似模拟、离散元数值模拟方法分析了厚硬基本顶采动破坏结构演化和堆积特征对覆岩下沉破坏的影响。相似模拟及数值模拟结果均表明,随采随垮的直接顶岩层和周期性破断的厚硬基本顶分别呈现小块度破坏杂乱堆积和大块度破断整齐堆积;受采动结构特征影响,直接顶岩层采动破坏产生的体积膨胀显著大于厚硬基本顶。根据模拟得到的采动岩层破坏堆积特征构建了厚硬基本顶条件下采动覆岩下沉计算模型。根据采动作用下随采随垮直接顶岩层采动破坏膨胀量显著大于周期性破断厚硬基本顶的规律,提出对厚硬基本顶进行采前大规模水力压裂并借助采动超前支承压力进一步破坏厚硬基本顶,降低厚硬基本顶采动破坏块度,使其随采随垮、杂乱堆积并充分充填采空区以控制上覆岩层下沉破坏,实现低损开采。采用数值模拟验证了压裂弱化厚硬岩层调控其采动结构,增大采动破坏岩层体积膨胀量,降低上覆岩层下沉的有效性。提出的厚硬岩层结构调控低损开采方法可为煤矿绿色高效开采提供一定的参考。

富水环境下盾构隧道最小覆盖层厚度设计与计算方法综述

覆盖层厚度设计是建设水下盾构隧道的关键环节之一。覆盖层厚度过小,围岩在施工扰动下易发生失稳,引起塌方、突水等灾害;覆盖层厚度过大,则会对工程预算与工期提出更高的要求。通过文献调研,结合已有实际水下盾构隧道工程案例,对现有合理覆盖层厚度设计和计算方法进行研究与总结。得出:1)水下盾构隧道设计方法主要分为理论分析法和数值模拟法;2)根据隧道结构稳定分析侧重点不同,理论分析法可分为考虑抗浮稳定性设计方法和考虑掌子面稳定性设计方法;3)现阶段水下盾构隧道合理覆盖层厚度的设计方法多基于数值模拟和理论分析,对实际工程工况进行一定程度的简化,且未能全面考虑复杂建(构)筑物环境、施工工艺以及隧道自身结构特性的影响,覆盖层厚度的研究深度和设计方法的适用性仍需进一步提高;4)目前,富水环境下盾构隧道最小覆盖层厚度的研究内容已较为丰富,但与实际工程的结合较为困难。未来的研究应进一步考虑施工的经济性、施工流程、复杂环境条件、结构寿命及智慧建造平台等方面。

不同时间添加蚯蚓对矸石覆土生理生态的影响

为探究不同时间添加蚯蚓对矸石覆土中香根草(Vetiveria zizanioides)生理生态的影响,采用土柱试验,设置两种覆土厚度[30 cm(M)、50 cm(N)],每组覆土分别设4个处理组:单独种植香根草(CK)、接种蚯蚓20 d后添加香根草(A)、同时接种蚯蚓和添加香根草(B)、添加香根草20 d后接种蚯蚓(C)处理,分析覆土理化性质及香根草生理生态指标变化特征。结果显示:与CK相比,A、B和C处理均能使覆土pH显著降低趋向中性(P<0.05),提升覆土电导率(EC)、有机质(OM)、全氮(TN)和全磷(TP)含量。与CK相比,不同时间接种蚯蚓均能增加香根草发芽率、总重和叶绿素a含量,其中B处理光合色素(叶绿素a、叶绿素b、类胡萝卜素)含量、A处理叶绿素b含量和C处理根系总长较CK均显著提高(P<0.05)。与CK相比,B处理降低香根草可溶性蛋白和脯氨酸含量效果较强,30和50 cm厚度覆土下B处理香根草可溶性蛋白较CK分别降低9.34%和4.69%(P<0.05),50 cm厚度覆土下脯氨酸含量较CK降低了5.55%(P<0.05),而A处理能显著提高香根草丙二醛含量。同一覆土厚度下,A处理仅在30 cm条件下显著降低香根草过氧化氢酶活性;B、C处理香根草超氧化物歧化酶、过氧化物酶活性较CK相比均无显著差异(P>0.05)。冗余分析和相关性分析表明:A、C处理中覆土OM、TN是影响香根草生理生态特性主要环境因子,而B处理中覆土OM、TP是影响香根草生理生态特性的主要环境因子。研究结果可为蚯蚓-香根草联合应用于复垦土壤修复提供理论依据。