时间重力测量,战役和永久GNSS以及干扰测量雷达技术:在得克萨斯州沿海地区量化土地变形速率的比较方法
Amanda Beattie1, Mohamed Ahmed1, Tianxing Chu2
1Department of Physical and Environmental Sciences, Texas A&M University-Corpus Christi, Corpus Christi, TX 78412, USA.
The Science of the total environment
|November 2, 2024
概括
德克萨斯州沿海曲地区的土地沉降率很高,工业区的土地沉降率高达-3.8毫米/年. 这项研究使用InSAR和GNSS量化了变形,为沿海弹性提供了见解.
科学领域:
- 地质科学 地质科学
- 环境科学 环境科学
- 遥感 遥感 遥感 遥感
背景情况:
- 沿海地区面临着土地沉降和海平面上升的重大威胁,导致洪水增加和基础设施损坏.
- 了解土地变形对于有效的沿海管理和减轻危险影响至关重要.
研究的目的:
- 用多种技术量化德克萨斯州沿海曲地区的土地变形率.
- 在地方和区域范围内调查土地沉降的控制因素.
- 评估不同地质测量方法的有效性,以监测土地变形.
主要方法:
- 活动利用了全球导航卫星系统 (GNSS) 和时间重力测量在六个地点两年.
- 在五年内使用交叉测量合成孔径雷达 (InSAR) 和15个永久GNSS站进行区域范围的分析.
- 比较来自重力,活动GNSS,InSAR和永久GNSS的数据,以评估测量的一致性和可靠性.
主要成果:
- 在SAR和永久GNSS数据显示了一致的土地变形速率 (分别从-12.16 ± 0.12到+11.70 ± 0.00毫米/年和-14.0 ± 0.6到+9.0 ± 3.0毫米/年),表明时空变化.
- 在沿海城镇,城市,内陆城镇和工业设施中观察到显著的沉降率,归因于沉积物凝结,断层和资源开采.
- 引力和竞选GNSS数据之间的不一致性被发现,可能是由于测量周期短和数据采集不频繁.
结论:
- InSAR和永久GNSS可靠地监测沿海地区的区域性土地沉降情况.
- 德克萨斯州沿海的土地沉降是由多种因素驱动的,包括自然过程和人为活动.
- 这些发现提供了关键数据,以提高当地海平面上升的估计,并支持沿海社区制定减缓和弹性战略.
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