地下深部多物理场观测与研究——淮南-848 m深试验。

IF 6 2区 地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY Science China Earth Sciences Pub Date : 2023-01-01 DOI:10.1007/s11430-022-9998-2
Yun Wang, Yaxin Yang, Heping Sun, Chengliang Xie, Qisheng Zhang, Xiaoming Cui, Chang Chen, Yongsheng He, Qiangqiang Miao, Chaomin Mu, Lianghui Guo, Jiwen Teng
{"title":"地下深部多物理场观测与研究——淮南-848 m深试验。","authors":"Yun Wang,&nbsp;Yaxin Yang,&nbsp;Heping Sun,&nbsp;Chengliang Xie,&nbsp;Qisheng Zhang,&nbsp;Xiaoming Cui,&nbsp;Chang Chen,&nbsp;Yongsheng He,&nbsp;Qiangqiang Miao,&nbsp;Chaomin Mu,&nbsp;Lianghui Guo,&nbsp;Jiwen Teng","doi":"10.1007/s11430-022-9998-2","DOIUrl":null,"url":null,"abstract":"<p><p>Compared with the surface, the deep environment has the advantages of allowing \"super-quiet and ultra-clean\"-geophysical field observation with low vibration noise and little electromagnetic interference, which are conducive to therealization of long-term and high-precision observation of multi-physical fields, thus enabling the solution of a series of geoscience problems. In the Panyidong Coal Mine, where there are extensive underground tunnels at the depth of 848 m belowsea level, we carried out the first deep-underground geophysical observations, including radioactivity, gravity, magnetic, magne-totelluric, background vibration and six-component seismic observations. We concluded from these measurements that (1) the background of deep subsurface gravity noise in the long-period frequency band less than 2 Hz is nearly two orders ofmagnitude weaker than that in the surface observation environment; (2) the underground electric field is obviously weaker thanthe surface electric field, and the relatively high frequency of the underground field, greater than 1 Hz, is more than two orders of magnitude weaker than that of the surface electric field; the east-west magnetic field underground is approximately the same asthat at the surface; the relatively high-frequency north-south magnetic field underground, below 10 Hz, is at least one order ofmagnitude lower than that at the surface, showing that the underground has a clean electromagnetic environment; (3) in additionto the high-frequency and single-frequency noises introduced by underground human activities, the deep underground spacehas a sig-nificantly lower background vibration noise than the surface, which is very beneficial to the detection of weakearthquake and gravity signals; and (4) the underground roadway support system built with ferromagnetic material interferesthe geomagnetic field. We also found that for deep observation in the \"ultra-quiet and ultra-clean\" environment, the existinggeophysical equipment and observation technology have problems of poor adaptability and insufficient precision as well asdata cleaning problems, such as the effective separation of the signal and noise of deep observation data. It is also urgent tointerpret and comprehensively utilize these high-precision multi-physics observation data.</p><p><strong>Electronic supplementary material: </strong>Supplementary material is available in the online version of this article at 10.1007/s11430-022-9998-2.</p>","PeriodicalId":21651,"journal":{"name":"Science China Earth Sciences","volume":"66 1","pages":"54-70"},"PeriodicalIF":6.0000,"publicationDate":"2023-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9782270/pdf/","citationCount":"1","resultStr":"{\"title\":\"Observation and research of deep underground multi-physical fields-Huainan -848 m deep experiment.\",\"authors\":\"Yun Wang,&nbsp;Yaxin Yang,&nbsp;Heping Sun,&nbsp;Chengliang Xie,&nbsp;Qisheng Zhang,&nbsp;Xiaoming Cui,&nbsp;Chang Chen,&nbsp;Yongsheng He,&nbsp;Qiangqiang Miao,&nbsp;Chaomin Mu,&nbsp;Lianghui Guo,&nbsp;Jiwen Teng\",\"doi\":\"10.1007/s11430-022-9998-2\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p><p>Compared with the surface, the deep environment has the advantages of allowing \\\"super-quiet and ultra-clean\\\"-geophysical field observation with low vibration noise and little electromagnetic interference, which are conducive to therealization of long-term and high-precision observation of multi-physical fields, thus enabling the solution of a series of geoscience problems. In the Panyidong Coal Mine, where there are extensive underground tunnels at the depth of 848 m belowsea level, we carried out the first deep-underground geophysical observations, including radioactivity, gravity, magnetic, magne-totelluric, background vibration and six-component seismic observations. We concluded from these measurements that (1) the background of deep subsurface gravity noise in the long-period frequency band less than 2 Hz is nearly two orders ofmagnitude weaker than that in the surface observation environment; (2) the underground electric field is obviously weaker thanthe surface electric field, and the relatively high frequency of the underground field, greater than 1 Hz, is more than two orders of magnitude weaker than that of the surface electric field; the east-west magnetic field underground is approximately the same asthat at the surface; the relatively high-frequency north-south magnetic field underground, below 10 Hz, is at least one order ofmagnitude lower than that at the surface, showing that the underground has a clean electromagnetic environment; (3) in additionto the high-frequency and single-frequency noises introduced by underground human activities, the deep underground spacehas a sig-nificantly lower background vibration noise than the surface, which is very beneficial to the detection of weakearthquake and gravity signals; and (4) the underground roadway support system built with ferromagnetic material interferesthe geomagnetic field. We also found that for deep observation in the \\\"ultra-quiet and ultra-clean\\\" environment, the existinggeophysical equipment and observation technology have problems of poor adaptability and insufficient precision as well asdata cleaning problems, such as the effective separation of the signal and noise of deep observation data. It is also urgent tointerpret and comprehensively utilize these high-precision multi-physics observation data.</p><p><strong>Electronic supplementary material: </strong>Supplementary material is available in the online version of this article at 10.1007/s11430-022-9998-2.</p>\",\"PeriodicalId\":21651,\"journal\":{\"name\":\"Science China Earth Sciences\",\"volume\":\"66 1\",\"pages\":\"54-70\"},\"PeriodicalIF\":6.0000,\"publicationDate\":\"2023-01-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9782270/pdf/\",\"citationCount\":\"1\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Science China Earth Sciences\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.1007/s11430-022-9998-2\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Science China Earth Sciences","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.1007/s11430-022-9998-2","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
引用次数: 1

摘要

与地表相比,深部环境具有“超安静、超洁净”的地球物理场观测优势,振动噪声低,电磁干扰小,有利于实现多物理场的长期高精度观测,从而解决一系列地球科学问题。在海拔848 m深的盘东煤矿,我们首次开展了深部地球物理观测,包括放射性、重力、磁力、大地电磁、背景振动和六分量地震观测。结果表明:(1)小于2 Hz长周期频带的深地下重力噪声背景比地面观测环境弱近2个数量级;(2)地下电场明显弱于地表电场,且地下电场的相对高频(大于1 Hz)比地表电场弱两个数量级以上;地下东西方向的磁场与地表大致相同;地下南北磁场相对高频,低于10 Hz,比地表磁场至少低一个数量级,说明地下电磁环境干净;(3)除了地下人类活动引入的高频和单频噪声外,地下深层空间的背景振动噪声明显低于地表,这对弱地震和重力信号的检测非常有利;(4)铁磁材料构成的地下巷道支护系统对地磁场的干扰。我们还发现,对于“超静超净”环境下的深度观测,现有的地球物理设备和观测技术存在适应性差、精度不够的问题,以及数据清洗问题,如对深度观测数据的信号和噪声进行有效分离。对这些高精度的多物理场观测数据进行解释和综合利用也十分迫切。电子补充资料:本文在线版本10.1007/s11430-022-9998-2提供补充资料。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Observation and research of deep underground multi-physical fields-Huainan -848 m deep experiment.

Compared with the surface, the deep environment has the advantages of allowing "super-quiet and ultra-clean"-geophysical field observation with low vibration noise and little electromagnetic interference, which are conducive to therealization of long-term and high-precision observation of multi-physical fields, thus enabling the solution of a series of geoscience problems. In the Panyidong Coal Mine, where there are extensive underground tunnels at the depth of 848 m belowsea level, we carried out the first deep-underground geophysical observations, including radioactivity, gravity, magnetic, magne-totelluric, background vibration and six-component seismic observations. We concluded from these measurements that (1) the background of deep subsurface gravity noise in the long-period frequency band less than 2 Hz is nearly two orders ofmagnitude weaker than that in the surface observation environment; (2) the underground electric field is obviously weaker thanthe surface electric field, and the relatively high frequency of the underground field, greater than 1 Hz, is more than two orders of magnitude weaker than that of the surface electric field; the east-west magnetic field underground is approximately the same asthat at the surface; the relatively high-frequency north-south magnetic field underground, below 10 Hz, is at least one order ofmagnitude lower than that at the surface, showing that the underground has a clean electromagnetic environment; (3) in additionto the high-frequency and single-frequency noises introduced by underground human activities, the deep underground spacehas a sig-nificantly lower background vibration noise than the surface, which is very beneficial to the detection of weakearthquake and gravity signals; and (4) the underground roadway support system built with ferromagnetic material interferesthe geomagnetic field. We also found that for deep observation in the "ultra-quiet and ultra-clean" environment, the existinggeophysical equipment and observation technology have problems of poor adaptability and insufficient precision as well asdata cleaning problems, such as the effective separation of the signal and noise of deep observation data. It is also urgent tointerpret and comprehensively utilize these high-precision multi-physics observation data.

Electronic supplementary material: Supplementary material is available in the online version of this article at 10.1007/s11430-022-9998-2.

求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
Science China Earth Sciences
Science China Earth Sciences GEOSCIENCES, MULTIDISCIPLINARY-
CiteScore
9.60
自引率
5.30%
发文量
135
审稿时长
3-8 weeks
期刊介绍: Science China Earth Sciences, an academic journal cosponsored by the Chinese Academy of Sciences and the National Natural Science Foundation of China, and published by Science China Press, is committed to publishing high-quality, original results in both basic and applied research.
期刊最新文献
Evaluation and attribution of trends in compound dry-hot events for major river basins in China Crustal growth and reworking at Archean plate margins Probing the interseismic locking state of the Xianshuihe fault based on a viscoelastic deformation model Global seismic tomography reveals remnants of subducted Tethyan oceanic slabs in the deep mantle A metallogenic model for the supergiant gold system in Jiaodong province: Constraints from crustal velocity structure
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1