利用点质量模型进行远程弹道重建。

Fabiano Riva, Frederick Richard Broekhuis, Michael Haag, Lambertus Koene, Wim Kerkhoff
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引用次数: 0

摘要

在枪击事件重建中,法医通常处理涉及短程轨迹的场景,通常≤30米。在这种情况下,线性轨迹重建模型是合适的。然而,法医专家也可以通过重建远程弹道来估计射手的位置,其中子弹的路径由于重力和更长的飞行时间而变成弧形。在本研究中,我们使用了点质量模型(PMM),因为它易于获取并且被认为足够精确。使用PMM的计算机程序可以从撞击点开始执行远程弹道重建。重建的结果是在一个预计射击的区域,而不是一个单一的地点。这是由改变PMM的输入参数引起的。本研究的目的是评估该方法的准确性,并讨论最相关参数的影响。通过将该模型的性能与使用多普勒雷达在远距离(即从500米至1800米)测量确定的20个手枪子弹轨迹进行比较,验证了该模型的性能。使用模型计算的面积与实际射手位置的比较表明了这些重建的局限性,特别是在高入射角时。重建的偏转量与跟踪雷达测得的偏转量差异较大。造成这种现象的原因可能是侧风作为高度函数的测量误差,也可能是雷达偏转测量的不准确。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Long-range trajectory reconstructions using the point mass model.

In shooting incident reconstructions, forensic examiners usually deal with scenes involving short-range trajectories, typically ≤30 m. In situations such as this, a linear trajectory reconstruction model is appropriate. However, a forensic expert can also be asked to estimate a shooter's position by reconstructing a long-range trajectory where the bullet's path becomes arced as a result of gravity and the greater time in flight. In this study, the point mass model (PMM) was used, because it is accessible and considered sufficiently accurate. A computer program using PMM can perform long-range trajectory reconstructions starting from an impact point. The reconstruction results in an area where the shot is expected to be fired from, not a single location. This is caused by varying the input parameters of the PMM. The aim of this study is to assess the accuracy of the method and discuss the influence of the most relevant parameters. The model has been validated by comparing its performance with 20 handgun bullet trajectories that were determined using Doppler radar measurements over long ranges, i.e. from 500 m to 1800 m. Comparison between the area calculated using the model and the actual shooter position demonstrates the limits of these reconstructions, particularly at high incident angles. The differences between the reconstructed deflections and the deflections measured by the tracking radar are rather large. This phenomenon is caused by either measurement errors in the cross wind as a function of height or inaccuracy of the radar's deflection measurements.

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