梳子坝淤砂形态特征试验研究

通过室内水槽试验,探讨梳子坝淤砂的形态特征、淤砂长度和回淤坡度等,初步得到:(1)梳子坝在全闭塞时,淤砂形态与实体坝相似,在淤砂区的前部,淤砂高度大致等于坝体高度,在淤砂区的尾部,都有一个明显的陡坎;梳子坝在部分闭塞时,淤砂形态与不闭塞情况下淤砂形态相似,在淤砂区的前部,都有一个缓坡。不闭塞时形成的缓坡坡度稍大于部分闭塞时的缓坡坡度,但都明显小于水下休止角,表明梳子坝淤砂形态异于狭缝坝。(2)梳子坝淤砂长度与切口宽度有关,大致有随着切口宽度的增大而减短的趋势;切口密度和泥石流浓度对淤砂长度有影响,淤砂长度有大致随切口密度的增大而堆积长度减短的趋势。(3)在相同试验条件下,梳子坝回淤坡度与实体坝相比大致相近,波动范围很小;在相同的切口宽度条件下,切口密度对回淤坡度有一定的影响,同时证明沟床坡度和泥石流的物质级配、容重及规模对回淤坡度也有一定影响。     

高海拔排土场边坡安全稳定性SBAS-InSAR监测

为解决高海拔排土场边坡安全稳定性监测中常规监测仪器布置和人员值守的高投入、高风险问题,分析西藏山南桑日县某排土场边坡25景Sentinel-1A数据,利用短基线集合成孔径雷达干涉测量(SBAS-InSAR)技术监测终了排土场边坡从2018年11月4日-2020年12月23日期间的地表形变,采用基线估计状态空间模型、自适...     

Influence of slope aspect on soil physico-chemical and biological properties in the mid hills of central Nepal

This study assessed the influence of slope aspect and land use on soil physio-chemical and biological properties (soil quality indicators) on contiguous south- and north-facing slopes of the mid hills in central Nepal, having the same climate, vegetation and parent material. In each aspect, two treatments (agriculture and forest) were chosen and four replicates taken for each treatment. Soil sample collection and microarthropod extraction was done according to the standard methodology: soil core samples (10 × 10 × 5 cm) and extraction with the modified Berlese–Tullgren funnel. The investigated soil variables were temperature, moisture, faunal abundance and diversity, organic matter, organic carbon, bulk density and pH. Except in a few cases, all considered soil properties showed significant differences between aspects and land use. Soils of the north-facing slope had higher SOC content, moisture, faunal abundance and diversity, and lower temperature and pH. Variations due to topographic aspect induced varied microclimates, causing differences in faunal abundance and diversity; soil moisture, temperature and organic matter trends affected soil fertility and ultimately soil quality. Further studies are required to clarify the complex interactions between soil properties (physio-chemical and biological), vegetation and slope aspect in Nepal, as well as to develop soil biological indicators as a tool to assist in sustainable land management.     

陕北黄土区陡坡土壤水分变异规律研究

土壤水分是制约陕北黄土区陡坡林草植被建设主要限制因素,深入系统的研究陡坡土壤水分变异规律是科学开展林草植被建设的重要前提。目前,陡坡不同季节、不同坡向、不同坡度的土壤水分变异规律尚未见系统的研究。为此,本研究通过观测陕北黄土区坡面尺度的自然恢复流域陡坡土壤含水量,研究分析了陡坡土壤水分季节变化规律、陡坡土壤水分垂直变化规律,结果表明：（1）陕北黄土区陡坡的土壤水分消耗期、土壤水分积累期、土壤水分消退期和土壤水分稳定期分别对应3-6、7-9、10-11和12月-次年2月;（2）0~120 cm土层中0~60 cm土层土壤含水量变化活跃。土壤水分随着土层深度的增加而增加,且各层间的差异也越来越显著;（3）基于土壤水分的垂直变化规律,陡坡的土壤水分弱利用层、土壤水分利用层、土壤水分调节层分别为0~40、40~60和60~100 cm。（4）在垂直于陡坡坡面方向上,深度大于40~50 cm的土壤层能为植被生长提供良好的土壤水分环境,有利于人工植被建设在陡坡开展。     

软弱基底排土场变形破坏治理措施研究

针对软弱基底露天矿排土场普遍存在的变形破坏问题,结合胜利东二露天矿南排土场南帮边坡的工程实际,基于极限平衡理论,给出了通过探槽及滑坡变形反分析综合确定基底赋存条件及抗剪强度指标的方法;提出了对软弱基底排土场的变形治理措施;根据已有监测数据,对南帮边坡治理效果进行了评价。结果表明:在实施削坡减载措施后,各地表监测点的累计位移趋于平缓,边坡治理措施效果明显,解决了胜利东二露天矿迫切的安全问题,为同样具有软弱基底的其他露天矿排土场变形及破坏治理提供了指导。     

Interspecific association among main plant species in the unstable slope with high-frequency debris flow北大核心CSCD

To determine the characteristics of vegetation community structure and the relationship between species in the frequent watersheds of debris flow in fragile ecological environments, based on sample survey and 2 × 2 joint table techniques, we used analysis of variance test, χ2 test, Jaccard index, Pearson correlation coefficient, and Spearman's rank correlation coefficient test to study the main plant species correlations in the stable zone, instable zone, and deposit zone of the unstable slope. The analysis of variance test showed that all 45 species pairs had a significant negative correlation in the stable zone and instable zone, whereas there was no significant negative correlation in the deposit zone, which showed that the species had an independent distribution trend. The results from the different tests showed that there were 1 pair, 4 pairs, and 4 pairs from the stable zone, instable zone, and deposit zone, respectively, which had significant interspecific association under the χ2 test and the ratios of positive correlation pairs to negative correlation pairs were 0.55, 0.67, and 0.67 in the stable zone, instable zone, and deposit zone, respectively. There were 8 pairs, 5 pairs, and 5 pairs from the stable zone, instable zone, and deposit zone, respectively, which had significant interspecific association from the Pearson correlation analysis test, and the ratios of positive correlation pairs to negative correlation pairs were 0.36, 0.45, and 0.45 in the stable zone, instable zone, and deposit zone, respectively. There were 10 pairs, 6 pairs, and 9 pairs from the stable zone, instable zone, and deposit zone, respectively, which had significant interspecific association from the Spearman's rank correlation analysis test and the ratios of positive correlation pairs to negative correlation pairs were 0.5, 0.55, and 0.6 in the stable zone, instable zone, and deposit zone, respectively. The three test results showed general similarities but there were some differences. Most species pairs did not reach a significant level in the three zones and the number of negatively related species was more than the number of positively related species. In brief, this loose interspecific relationship indicates that the entire plant community was not stable, and the interspecific relationships among species are susceptible to environmental interference in the ecologically fragile areas of the debris flow basin. Therefore, rational selection and configuration of species should be applied to promote community structure development and ecological environmental improvement in vegetation restoration process areas with high-frequency debris flow. © 2018 Science Press. All rights reserved.     

岩质高边坡运营安全风险评估指标体系研究

为建立高速公路岩质高边坡风险评估指标体系,针对指标选取代表性不足、指标分级阈值缺少定量判据、指标获取困难等问题,采用逐坡普查与重点调查、工程地质类比与复核、现场监测与数值计算相结合的方法,提出了岩质高边坡运营安全风险评估指标体系。包括边坡断面几何特征、水的影响、边坡岩体结构、支挡加固设施及边坡破坏模式等5个一级指标与坡高、坡度等15个二级指标,并确定了量化分级标准与取值方法。评估结果表明:指标体系适用性较强,为后续评估运营安全风险奠定了基础。     

坡度和植被盖度对河岸坡面侵蚀产沙特征的影响

坡度和植被盖度是影响坡面土壤侵蚀的重要因子,探讨坡面土壤侵蚀产沙对坡度和植被盖度的响应,对坡面土壤侵蚀产沙的预测和调控具有重要意义。研究基于野外模拟径流冲刷试验,分析了不同坡度（5°、10°、15°、20°）和植被盖度（0、15%、30%）条件下坡面径流系数、泥沙量、时段径流含沙量和侵蚀泥沙粒径组成的变化过程,并运用双因素方差分析和相对贡献指数阐明黄河下游河岸坡面侵蚀产沙特征对坡度和植被盖度交互作用的响应。结果表明：不同植被盖度下坡面径流系数随冲刷历时增加而增加,在冲刷历时前5 min增幅较快,之后增幅变慢并趋于平缓;坡面径流含沙量随冲刷历时呈逐渐下降趋势,随后趋于平缓。坡度小于15°时,不同植被盖度之间的径流系数和时段径流含沙量差异较为明显,坡度大于15°后差异减小。侵蚀产生的泥沙量随冲刷历时和坡度的增加而增加;在同一坡度上,植被覆盖越低,侵蚀产生泥沙量越大。侵蚀泥沙的主要富集粒级中,Dx(10)以粉粒为主,Dx(50)以粗粉粒和极细砂粒为主,Dx(90)以极细砂粒和细砂粒为主。双因素方差分析表明,坡度对河岸坡面侵蚀产生的径流系数、产沙量和径流含沙量均有极显著影响（P<0.001）,植被盖度对产沙量和径流系数有极显著影响（P<0.001）,而坡度和植被盖度的交互作用仅对径流系数有显著影响（P<0.01）,同时相对贡献指数表明,在坡度和植被盖度对坡面侵蚀产沙的交互作用中,植被盖度的作用随坡度的增加逐渐减弱,而坡度的作用逐渐增强,并成为影响坡面水土流失的主导因素。     

云南昭通市坡地聚落空间特征及其成因机制研究

坡地聚落是我国山区聚落的重要类型,多处于生态条件差、经济落后的山区。随着国家主体功能区规划进入实施阶段,充分认知坡地聚落面临的生态、贫困、聚落重组、人口迁居等问题具有重要的现实意义。论文以云南省昭通市为研究地区,运用GIS方法详尽探讨其坡地聚落的空间特征,并从区域发展视角分析坡地聚落空间特征的成因机制。研究表明:昭通市具有坡地聚落比例高、聚落密度突出、聚落分散布局、人类活动强度高、民族聚落垂直分异等显著特点。特殊的区位、人口基数和高人口增长率导致了高密度的聚落分布;生态脆弱、贫困和单一的农业生产方式加剧了人类活动强度;低城镇化工业化水平、有限的城市集聚力与欠发达的商品经济是聚落分散态势的重要成因。     

含地下采空区岩质边坡的施工过程数值分析

为研究含地下采空区的岩质边坡在施工过程中的各种响应与稳定性,采用SURPAC建立某磷矿的三维地质模型。在边坡坡顶、坡角与采空区四周布置应力与位移监测点。利用接口程序将三维模型导入FLAC3D,计算露天边坡开挖过程中监测点的应力与位移。计算结果表明:坡顶与坡角水平位移与竖向反弹位移随着边坡开挖的进行越来越大,但每步开挖完成后新增的反弹位移越来越小,这与每步开挖的卸载量大小有关。坡顶监测点处于拉应力状态,坡角监测点处于压剪应力状态,在监测点所在位置开挖时,压应力显著变大。地下空区的开挖过程对空区的竖向位移与应力有极大影响,最大主应力在每步开挖完成时突然增加,且增幅很大。建议在施工过程中,加强对采空区与边坡坡顶及坡脚的位移与应力的量测,以确保施工安全。