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椭球膨胀法在高海拔地区建立独立坐标系的应用

王振方

王振方. 椭球膨胀法在高海拔地区建立独立坐标系的应用[J]. 岩土工程技术, 2025, 39(3): 398-402. doi: 10.20265/j.cnki.issn.1007-2993.2024-0206
引用本文: 王振方. 椭球膨胀法在高海拔地区建立独立坐标系的应用[J]. 岩土工程技术, 2025, 39(3): 398-402. doi: 10.20265/j.cnki.issn.1007-2993.2024-0206
Wang Zhenfang. Ellipsoid expansion method in establishing independent coordinate system in high-altitude area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2025, 39(3): 398-402. doi: 10.20265/j.cnki.issn.1007-2993.2024-0206
Citation: Wang Zhenfang. Ellipsoid expansion method in establishing independent coordinate system in high-altitude area[J]. GEOTECHNICAL ENGINEERING TECHNIQUE, 2025, 39(3): 398-402. doi: 10.20265/j.cnki.issn.1007-2993.2024-0206

椭球膨胀法在高海拔地区建立独立坐标系的应用

doi: 10.20265/j.cnki.issn.1007-2993.2024-0206
详细信息
    作者简介:

    王振方,男,1982年生,硕士,高级工程师,主要从事工程测量工作。E-mail:wzf0373@126.com

  • 中图分类号: P226

Ellipsoid expansion method in establishing independent coordinate system in high-altitude area

  • 摘要: 分析工程控制网投影长度变形产生的原因及消除长度变形的方法,详述椭球膨胀法原理和计算椭球长半径变化量的4种方法。以高海拔地区某工程GNSS控制网为实例,采用平均曲率半径法、卯酉曲率半径法、平面解析法、广义微分法4种不同的椭球长半径变化量计算方法建立独立坐标系,比较分析4种方法计算得出的椭球长半径变化量、控制点的纬度及大地高变化量,全站仪实测距离的验证结果表明4种计算方法获得的高斯平面坐标精度基本一致,但平面解析法与广义微分法最严密,结论可为高海拔地区建立独立坐标系提供参考。

     

  • 表  1  椭球长半轴改变量

    平均曲率半径法卯酉曲率半径法平面解析法广义微分法
    椭球长半轴改变量/m3855.48465343846.27717173853.72644243853.7264317
    下载: 导出CSV

    表  2  测区中心点及5个控制点的纬度及大地高变化量

    点号 变化量 平均曲率半径法 卯酉曲率半径法 平面解析法 广义微分法
    中心点纬度/(″)0.189308770.188856670.189222440.18922244
    大地高/m−1.756521567.44205677−0.000010770.00000000
    K1纬度/(″)0.189337030.188884870.189250690.18925069
    大地高/m−1.754630287.443943530.001879650.00189042
    K2纬度/(″)0.189322700.188870570.189236360.18923636
    大地高/m−1.755589697.442986410.000920670.00093144
    K3纬度/(″)0.189316720.188864600.189230380.18923038
    大地高/m−1.755989897.442587170.000520660.00053143
    K4纬度/(″)0.189296740.188844670.189210420.18921042
    大地高/m−1.757325687.44125456−0.00081453−0.00080376
    K5纬度/(″)0.189270620.188818610.189184300.18918430
    大地高/m−1.759071777.43951265−0.00255982−0.00254905
    下载: 导出CSV

    表  3  首级控制点的高斯平面坐标与CGCS2000下的高斯平面坐标差值

    方法K1K2K3K4K5
    ΔX/mΔY/mΔX/mΔY/mΔX/mΔY/mΔX/mΔY/mΔX/mΔY/m
    平均曲率半径2181.218−2.0652180.902−2.0262180.772−1.4902180.333−1.6062179.759−1.730
    卯酉圈半径法2176.022−2.0602175.708−2.0212175.578−1.4862175.140−1.6022174.567−1.725
    平面解析法2180.225−2.0642179.910−2.0242179.780−1.4892179.340−1.6052178.767−1.728
    广义微分法2180.225−2.0642179.910−2.0242179.780−1.4892179.340−1.6052178.767−1.728
    下载: 导出CSV

    表  4  控制点间反算距离与实测距离对比表

    距离起始点不同坐标系下控制点间的反算距离/mS0(全站仪实测距离)/m(S1-S0)
    /m
    (S2-S0)
    /m
    (S3-S0)
    /m
    (S4-S0)
    /m
    S1(平均曲率半径法)S2(卯酉圈半径法)S3(平面解析法)S4(广义微分法)
    K1—K2525.179525.178525.179525.179525.187−0.008−0.009−0.008−0.008
    K2—K3914.726914.724914.725914.725914.742−0.016−0.018−0.017−0.017
    K3—K4750.893750.892750.893750.893750.9050.0080.0070.0080.008
    K4—K5969.721969.719969.721969.721969.739−0.018−0.02−0.018−0.018
    下载: 导出CSV
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出版历程
  • 收稿日期:  2024-05-15
  • 修回日期:  2024-08-27
  • 录用日期:  2024-10-29
  • 刊出日期:  2025-06-09

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