地质灾害治理方案.pdf
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1、学习文档仅供参考地质灾害防治方案一、工程概况1、号站号站位于丰和路路中,沿丰和路南北向布置;车站东侧为丰和园小区和三官庙农贸市场、车站西侧叶语田园小区和新泉佳苑小区;车站位于道路中间,丰和路规划道路宽 40m。车站为 11m站台地下二层岛式车站,车站结构采用半盖挖法施工。车站起点里程右 K14+203.81,终点里程为 K14+662.41,车站长度约 458.4m,车站宽度约19.7 23.8m,底板埋深约 16.61m。车站共设 8 个出入口,3 个安全出口,4 组风亭。2、号站号站区间区间线路出号站后沿丰和路向前敷设,在丰和路与立交路交叉口东北角向东拐入南京路,之后沿南京路向东敷设,最后
2、进入位于南京路南侧的号站。区间长度为 984.28m,隧道采用盾构法施工。3、号站号站位于南京路与三环东路Y形交口东侧,梅花园小区北侧的地块内,沿南京路东西向设置。车站为 11m站台地下二层岛式车站。车站结构采用明挖顺筑施工。车站起点里程 K15+646.690,终点里程为 K15+885.490,车站长度约 238.8m,车站宽度约19.7 24.1m。车站共设 3 个出入口,两组风亭。4、号站号站区间区间线路由号站引出后,沿南京路布设,之后下穿绿地到达文博园园站。区间长度为 1304.980m,采用盾构法施工。学习文档仅供参考二、线路区地质环境特征1、地形地貌市区位于鲁南山区向黄淮海平原过
3、渡的部位,以平原为主,中部斜插丘陵山带,区内山体最大海拔标高153.00m,一般标高 100.00m 左右。山体坡角一般为 1535。平原是黄淮平原的一部分,其中黄河故道地势较高,海拔标高 36.0042.00m,其余地势低平,海拔标高32.0036.00m,自北西向南东微倾斜。根据地貌的分类原则:形态+成因+微地貌特征,市区内的地貌形态主要有丘陵残丘和平原两大类,前者是剥蚀-溶蚀作用的结果,后者是堆积作用的结果。号站和到号站位于冲积平原地貌单元,地势较平坦。附图 1图 1市地区区域地质构造图2、地层岩性及工程地质条件覆盖层均为第四系全新统人工堆积物 Q4ml 、第四系全新统冲积层Q4al、第
4、四系晚更新冲积层 Q3al,场地内均匀分布,厚度随地表起伏有所不同;下伏基岩奥陶系石灰岩等。结合地貌特征,勘察场区地层自上而下依次为:1-1 层杂填土 Q4ml 1-2 层素填土 Q4ml 2-3-1 层淤泥质黏土 Q4al2-3-2 层黏土 Q4al 2-5-3 层粉土 Q4al 5-3-4 黏土 Q3al 11-2-2 层强风化石灰岩O1m+x 文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10
5、I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码
6、:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3
7、A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S1
8、0 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K
9、8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K
10、7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T
11、5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3学习文档仅供参考11-2-3 层中风化石灰岩 O1m+x 11-2-3A 层破碎中风化石灰岩 O1m+x 3、水文地质条件工程线沿线区域地下水类型主要为潜水孔隙水 和承压水 碳酸盐裂隙岩溶水。潜水,为第四系松散层孔隙水,水位埋深 1.8 3.50m,水位标高 29.3530.45m,含水层主要为粉土 2-5-3 层及杂填土 1-1 层,局部位于黏土 2-3-2 层里。主要接受大气降水补给和侧向径流补给,以蒸发、侧
12、向径流、人工开采方式排泄。地下水动态季节性变化显著,一般在每年的5 月下旬至 6 月上旬,到达最低点;7、8 月是降雨高峰期,地下水位迅速上升到达最高点,变化幅度约为 1.0 2.0m。承压水,属于碳酸盐岩裂隙岩溶水,主要贮存于灰岩裂隙中。本次设置两个观测孔,观测结果显示,D2S13XZ16 号孔该层地下水稳定水头埋深6.35m,稳定水头标高 25.93m,D2S13CZ10 未观测到水位。说明场地内裂隙岩溶水的透水性和富水性取决于基岩裂隙的发育程度和裂隙的充填情况。裂隙岩溶水补给来源主要是大气降水入渗补给和侧向径流补给;径流在丘陵区受地形控制,由高处流向地处平原区,但在平原区受人工开采影响,
13、岩溶水表现为由四周流向开采降落漏斗中心的汇流型径流,水力度较大;排泄以人工开采为主。地下水动态一般每年雨季降水高峰期后一到两个月8、9 月岩溶水到达最高点,随后水位逐渐下降,至次年旱季末 4、5 月水位下降至最低点,年变幅在5.0 10.0m。附图 2文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:C
14、N1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6
15、L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10
16、HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J
17、6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7
18、ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X
19、6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3
20、文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3学习文档仅供参考图 2市地区区域水文地质图三、工程建设引发或遭受的地质灾害类型1、地面塌陷及地面沉降 根据岩土工程勘察报告地质剖面图可知,区间隧道结构顶板随隧道起伏穿过的土层依次为:黏土 5-3-4 层、中风化灰岩 10-1-3 层、全风化页岩 10-7A-1层、全风化页岩10-7B-1 层、全风化灰岩 11-1-1 层。结构位于穿越软硬不均地层,软硬不均导致围岩稳定性差,开挖后自稳时间短,易发生坍塌现象。盾构机位于黏性土层中时,围岩稳定性较差;该层黏土粘粒含量较大,初始掘进速度较快,但易造成刀盘处聚集泥饼,掘
21、导致进速度急剧下降;本区间多次穿越软硬不均地层,软硬不均会导致掘进速度下降。在上软下硬地层盾构掘进速度的下降会导致上方土体流失过多造成坍塌和地面下沉等情况。号站在采空区附近,受煤矿开采形成的塌陷区终采时间较长,且采空塌陷区域被处理,后期施工可能会遭受采空地面塌陷地质灾害危险;岩溶地层,岩溶洞隙上存在一定厚度的土层,在地下水频繁作用下,形成土洞进而引起地面塌陷,影响地铁结构基础稳定;构筑物底板下岩体破碎或存在溶沟、溶蚀裂隙、溶洞,同时随着时间推移,在溶蚀作用下,它们的规模会进一步扩大,可能影响构筑物基础稳定。施工过程中对基底土层的扰动、爆破震动以及地下水控制或其他因素引起的水位波动,将增加诱发岩
22、溶塌陷的风险;盾构机掘进过程中经过岩溶地质时,如有空洞会导致盾构机刀盘沉降等险情 特殊性粘土,填土 1-1 层,成分复杂,力学性质较差,易坍塌;黏土 2-3-3层,软塑可塑,局部夹粉土层,自稳能力差,受扰动后力学性质较差,易坍塌;黏土 5-3-4 层具有弱 中等膨胀性,其胀缩具有可逆性,地铁工程的施工周期较长,一般会经历雨季、旱季,容易使土体中含水量发生反复变化,造成膨胀土的反复胀缩变形,土体在胀缩变形过程中能产生较高的膨胀力,造成围岩压力增大,增加支护结构的受力,造成围岩失稳。2、涌水、涌砂灾害文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN
23、1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L
24、3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 H
25、B6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6E8K7 ZL8T5X6S10I3文档编码:CN1L3A6L3S10 HB6K8J6
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