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航空地球物理勘查科技创新与应用

熊盛青

熊盛青, 2020. 航空地球物理勘查科技创新与应用. 地质力学学报, 26 (5): 791-818. DOI: 10.12090/j.issn.1006-6616.2020.26.05.063
引用本文: 熊盛青, 2020. 航空地球物理勘查科技创新与应用. 地质力学学报, 26 (5): 791-818. DOI: 10.12090/j.issn.1006-6616.2020.26.05.063
XIONG Shengqing, 2020. Innovation and application of airborne geophysical exploration technology. Journal of Geomechanics, 26 (5): 791-818. DOI: 10.12090/j.issn.1006-6616.2020.26.05.063
Citation: XIONG Shengqing, 2020. Innovation and application of airborne geophysical exploration technology. Journal of Geomechanics, 26 (5): 791-818. DOI: 10.12090/j.issn.1006-6616.2020.26.05.063

航空地球物理勘查科技创新与应用

doi: 10.12090/j.issn.1006-6616.2020.26.05.063
基金项目: 

国家重点研发计划 2017YFC0602200

国家高技术研究发展计划(863计划) 2013AA063905

详细信息
    作者简介:

    熊盛青(1963-), 男, 教授级高级工程师, 主要从事航空地球物理、遥感技术及其地学应用研究工作。E-mail:xsqagrs@126.com

  • 中图分类号: P631

Innovation and application of airborne geophysical exploration technology

  • 摘要: 简要回顾了中国航空物探技术的发展历程,重点阐述了21世纪以来、尤其是"十一五"以来国内航空物探的主要技术创新与应用成果,并对今后发展趋势进行了分析与预测。为满足国家与社会需求,"十一五"以来,中国的航空物探技术,尤其是航磁多参量、矢量测量、航空重力测量和时间域航空电磁测量技术得到快速发展;在航空物探技术创新过程中,航空物探资料的综合研究和应用得到了加强,在基础地质、固体矿产勘查与评价、能源勘查与评价等方面取得了重要成果,在地下水资源调查、工程地质勘查、环境地质调查等方面显示出了良好的应用前景。为满足国家资源勘查和环境评价对航空探测技术的需求,未来中国航空物探测量系统的分辨率、稳定性和实用性将进一步提高,航空物探在加强基础地质、固体矿产勘查、能源勘查等传统领域应用的基础上,将拓展及加强在深地探测、深海探测、深部地热调查、水资源调查、地质灾害调查、军事及测绘等领域的应用。

     

  • 图  1  自主研制航空物探仪器装备及其技术指标的标志性进展

    Figure  1.  China's airborne geophysical exploration instruments and the landmark progress of technical indicators

    图  2  高分辨综合航空地球物理勘查技术体系

    Figure  2.  Technical system of the high resolution integrated airborne geophysical exploration

    图  3  中国陆域航磁ΔT化极立体阴影图(Xiong et al., 2016a)

    Figure  3.  Stereo shaded-relief image of aeromagnetic ΔT data of continental China with magnetic pole reduction. (Xiong et al., 2016a)

    图  4  中国陆域磁性基底深度图(Xiong et al., 2016a)

    Figure  4.  Magnetic basement depth map of continental China (Xiong et al., 2016a)

    图  5  中国陆域断裂及岩浆岩分布图(Xiong et al., 2016a)

    Figure  5.  Distribution of faults and magmatic rocks in continental China based on aeromagnetic data (Xiong et al., 2016a)

    图  6  中国陆域居里面深度图(熊盛青等,2016b)

    Figure  6.  Depth map of curie surface in continental China (Xiong et al., 2016b)

    图  7  曹妃甸地区不同深度电阻率切片(He et al., 2019)

    Figure  7.  Resistivity slices corresponding to elevation levels in Caofeidian area (He et al., 2019)

    图  8  航空地球物理勘查科学技术体系建设框图

    Figure  8.  Flow chart for the construction of science and technology system of airborne geophysical exploration

    表  1  航空物探方法的理论基础、物理性质及探测对象

    Table  1.   Theory, physical properties and detection objects of the airborne geophysical exploration methods

    方法 理论基础 物理性质基础 测量对象
    航空磁测 毕奥-萨伐尔定律 磁化率、磁化强度差异 磁场
    航空重力测量 牛顿万有引力定律 密度差异 重力场
    航空电磁测量 麦克斯韦方程 导磁性、导电性差异 电磁场
    航空放射性测量 放射性同位素衰变 衰变常数差异 伽马能谱
    下载: 导出CSV

    表  2  国内外航空地球物理勘查系统核心仪器关键指标对比表

    Table  2.   Comparison of key indicators of domestic and foreign airborne geophysical exploration systems

    装备 技术指标 当前国际 当前国内 评价
    航空磁测系统 总场 灵敏度/pT ±0.35 ±0.3 先进
    灵敏度/pT ±0.5 ±0.3
    梯度 水平梯度噪声/(pT/m) 5 2 先进
    垂向梯度噪声/(pT/m) 20 10
    三分量 噪声/nT 60 3 领先
    张量梯度 噪声/(pT/m) 5 / 差距大
    航空重力测量系统 总场 测量精度/mGal ±0.6 ±0.6 先进
    静态精度/mGal ±0.01~±0.1 ±0.1
    梯度 测量精度/E ±1~±5 / 差距大
    直升机航空电磁系统 TEM 发射磁矩/Am2 1.3×106 3.5×105 先进,有差距
    动态噪声/(nT/s) ±1 ±2
    勘探深度/m 500~800 300~400
    大地电磁 动态范围/dB 130 / 差距大
    系统噪声/fT 30 /
    探测深度/km 1~3 /
    航空伽马能谱测量系统 能量分辨率/%(137Cs) 8.0 4.0 先进
    峰漂/道 < 1 < 0.5
    起始能量/keV 50~70 < 20
    注:组成上述系统的仪器,除航空磁力仪、重力仪、电磁仪和伽马能谱仪等核心仪器外,还包括:磁干扰场补偿器、磁日变观测系统、数据收录仪、专用导航系统、综合定位数据采集系统、仪器供电适配系统等配套仪器与设备,中国均实现了自主研制,并保持与国外同等先进水平
    下载: 导出CSV

    表  3  中国不同时期航空地球物理勘查技术对比表

    Table  3.   Comparison of airborne geophysical exploration techniques of different periods in China

    内容 第一代(20世纪50年代初期—20世纪80年初期) 第二代(20世纪80代中期—20世纪90年中期) 第三代(20世纪90年代末期—现在) 第三代主要进步
    勘查方法 航磁(总场)、航空放射性(伽马总量、后期4道伽马能谱)、航空电磁(频率域) 航磁(总场、水平梯度)、航空放射性(伽马能谱,4道、512道)、航空电磁(频率域) 航磁(总场、全轴梯度、矢量)、航空放射性(伽马能谱,512道、1024道)、航空电磁(频率域、时间域)、航空重力 实现全部4类方法勘查应用
    测量仪器 引进为主, 部分自研 航磁自研,其它引进 自主研制与引进结合 自主研制各类仪器,主要技术指标与国外相当,并工程化应用
    测量参量 4~11个:航磁(1),航空伽马(1)和伽马能谱(4),频率域航电(2-6) 13个:航磁(3)、三频航电(6)、航空伽马能谱(4) 42个:航磁(10)、航电(频率域12+时间域15)、航空伽马能谱(4)、航空重力(1) 增加29个
    飞行平台 固定翼飞机、直升机 固定翼飞机、直升机 多型固定翼飞机、直升机、无人机、滑翔机、飞艇 多样化,全地域测量能力
    测量比例尺 1:100万—1:20万为主,部分1:10万,最大1:5万 1:20万、1:10万为主,部分1:100万、1:5万,最大1:2.5万 1:5万为主,部分1:20万和1:10万,最大1:4000 提高5倍以上,实现高分辨、精细化探测
    导航定位 地形图目视领航;后期多普勒导航等;布标+照相定位、后期部分应答定位等,定位精度约1 km~n×100 m 仪表导航,后期GPS、GLONASS导航定位为主;
    定位精度±n×100~±10 m
    GPS和DGPS导航定位;
    定位精度±10~±1 m
    三维自主导航;
    定位精度提高5倍以上
    高度测量 人工记录气压高度, 后期中低精度无线电测高仪 数字气压高度, 无线电测高 GPS高度、高精度无线电测高 精度达到米级
    数据收录方法 模拟曲线记录 微机数字收录/模拟曲线记录 完全数字收录 软件国产化、全流程数字化
    资料处理解释与成图方法 人工、半机械整理,手工清绘成图,成果为纸介质 引进专用软件处理、解释、成图,成果以纸介质为主 国产专用软件处理、解释、成图,数字化成果
    测量精度 低—中精度(磁测精度±100~±5 nT) 高精度(磁测精度±5~±3 nT) 高精度(磁测精度±3~±1 nT;航空重力±1.0 mGal) 磁测精度提高2~3倍
    应用领域 以找铁矿、铀矿和圈油气盆地与局部构造为主 固体矿产与油气勘查、区域地质调查、地球深部结构探测、地下水资源调查等 固体矿产与油气勘查、区域地质调查、地球深部结构探测、地下水资源调查、工程地质勘查、环境评价、军事地质、测绘、核应急监测等 应用领域更广
    注:分代时间在前人的基础上进行了适当调整
    下载: 导出CSV

    表  4  不同航空物探方法的主要用途及相应的测量比例尺

    Table  4.   Main application of different airborne geophysical methods and corresponding measurement scales

    方法 主要用途 局限性 测量比例尺 备注
    航空磁测 铁矿、多金属和非金属矿、油气勘查,区域地质调查,工程地质勘查,地球深部结构探测、军事等 垂向分辨率较低 1:4000—1:20万 可有以下几种不同组合:如重/磁、磁/伽马能谱、磁/电磁、磁/电磁/伽马能谱,等等。
    航空重力测量 油气、固体矿产勘查,区域地质调查,地球深部结构探测,军事,测绘等 目前空间分辨率难于满足固体矿产勘查 1:5万—1:20万
    航空电磁测量 矿产勘查、地下水资源调查、环境评价、地下电性结构探测等 易受电性干扰,探测深度受环境电阻率影响 1:4000—1:5万
    航空放射性测量 铀矿、稀土稀有金属矿、钾盐矿、多金属和非金属矿勘查,区域地质调查,环境辐射评价,核应急监测等 固体矿产调查局限于浅地表 1:2.5万—1:5万
    下载: 导出CSV
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  • 收稿日期:  2020-08-02
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