impact crater experiment results

As Earth has an active atmosphere with weather, these craters can easily become lost because of weathering. If the class is familiar with the equations of motion for constant acceleration (SUVAT equations), it would be possible to get them to plot impact speed against crater size instead. According to the qualitative relationship between the crater efficiency and the dimensionless strength, the lower the strength of the material is, the greater the final crater volume is. As shown in Figure, The third zone is the radial crack area. However, with the increase of the kinetic energy, the shape of the impact crater is no longer regular. Schematic diagram of the experimental system for a two-stage light gas gun. 5) Drop the first rock from a height of 30 cm Yanyu Qiu, Songlin Yue, Mingyang Wang, Gan Li, Yihao Cheng, Zhangyong Zhao, Zhongwei Zhang, "Experimental Investigation of the Crater Caused by Hypervelocity Rod Projectile Impacting on Rocks", Shock and Vibration, vol. is called dimensionless strength, and it is the ratio of target material strength to initial dynamic pressure. Both the measured μ-values are greater than 2/3. The front of the meteor hits the Earth, compressing the ground below it, and the back moves towards the front, compressing the entire body at an immense pressure. As shown in Figure 3, granite blocks are enclosed by C30 concrete and placed in a steel barrel. After each experiment, the morphology and size of the hypervelocity impacting crater were accurately obtained by using a device for image scanning. In addition, the dimensionless terms and are constant for given materials of the projectile and the target. The statistics in Table 1 are the experiment results. As shown, both the experimental results of this article and the experimental results by Lange et al. From Figure 15, the fitting curves of the relation between dimensionless ΠV and ΠY are shown as follows: From Figure 16, the fitting curves of the relation between dimensionless πV and πY are shown as follows: Combining Figures 15 and 16 and equations (24) and (25), it can be concluded that the relation between dimensionless ΠV and ΠY based on the energy scale are the same as the relation between dimensionless πV and πY based on the momentum scale. There were no tensile cracks on the edge of the rock target, which indicated that the target was large enough to be considered as a semi-infinite target without being affected by the boundary reflection wave. Animation of the formation of the Chicxulub crater (Credit – University of Arizona, Space Imagery Center). A simple case occurs for a final crater geometry measure such as the volume V. Therefore, it is given by a form such as, In a length-force-time system, the independent and dependent variables were developed according to dimensional analysis [21]. The pressure of the shockwave can change the structure of the rocks around the impact crater. The authors declare that there are no conflicts of interest regarding the publication of this paper. This is because the increase of the kinetic energy leads to much more increase of the diameter of the crater. With the increase of the projectile kinetic energy, it is uncertain whether the depth of the crater increases, but the volume of the crater will increase. Here, we present results of a series of impact experiments into porous wet and dry sandstone targets. Show and explain what shape an impact crater is and why. and Li and Chen [22, 23], , 43 which is widely known as the dimensionless impact factor or dimensionless energy factor. 6) Carefully remove the rock from the sand without damaging the impact crater This expression involves five quantities and three independent dimensional units and can therefore be written in terms of two dimensionless variables in various, but equivalent, ways. Comets are made of rock fragments held together by ice. Explosive processes,”, K. A. Holsapple and R. M. Schmidt, “On the scaling of crater dimensions: 2. Thus, let the dimensions of C be given by (length)l (velocity)μ (mass density)φ, where μ and φ are constants for given materials. Relation between the dimensionless diameter and the dimensionless depth. It is reasonable that the processes which lead to the final crater are strongly influenced by low-stress material properties and for large craters, by gravity. However, less success had been achieved in predicting the final crater size. Part I: engineering model for the mass loss and nose-blunting of ogive-nosed projectiles,”, H. Wu, Q. Chen, and L.-L. Relation between the kinetic energy of the projectile and the volume of the final crater. An interesting phenomenon was discovered that both small-scale impact craters in the laboratory and bowl-shaped craters which are less than 5 km in diameter on the Earth are controlled by strength (of rocks) [8]. Show and explain how the size of the ‘mini crater’ in the sand changes when a rock is dropped from a low or high altitude. 2020, Article ID 9768745, 11 pages, 2020. https://doi.org/10.1155/2020/9768745, 1School of Mechanical Engineering, Nanjing University of Science and Technology, Nanjing 210094, China, 2State Key Laboratory for Disaster Prevention & Mitigation of Explosion & Impact, College of Defense Engineering, Army Engineering University of PLA, Nanjing 210007, China. We are committed to sharing findings related to COVID-19 as quickly as possible. It is a movie of an experimental vertical impact at the NASA Ames Research Center. It shows that the depth of the crater is much smaller than the diameter of the crater, and the crater seems to be a shallow dish. The concepts of the transient crater and final crater are very important for brittle media such as rocks. (4)The volume of the transient and final crater increases with the increase of the projectile kinetic energy, and the contribution of spallation to the volume is growing more rapidly. The Vertical Impact Stack file is a movie made of a stack of 24 individual images, or frames. With μ = −1/3 and φ = 1/3, it has the units of (momentum)1/3. As it is shown in Figure, The second zone is the spallation area. Some interesting conclusions can be drawn from Figure 9: (1) the depth of the crater which is caused by the rod projectile (in this article) is 1-2 times of the length of the projectile, while the depth of the crater caused by the spherical projectile is 3–10 times of the length of the projectile. Lastly, dimensionless analysis of the impact crater was carried out. Asteroids are made of rock and metal; most are found orbiting the Sun between Mars and Jupiter. If the class is not comfortable data graphs, it would be possible to simply relate the idea that bigger rocks make bigger craters. Smaller objects do not burn up or slow down on bodies without atmospheres; hence, they may cause many more small impact craters than on Earth. In 1992, the Peekskill Meteor was seen travelling over much of the east coast of America, before landing on a car, damaging its bodywork Their formation can be separated into three stages The target is assumed to be initially in lithostatic equilibrium under the influence of gravitational field strength (). They should: 1) Smooth the sand down Equation (14) can be transformed as follows:where ; , which is the crater efficiency, and it is the volume ratio of the crater to the projectile; and , which is the dimensionless strength, and it is the ratio of initial dynamic pressure to material strength; it is obvious that ΠV and ΠY are power exponential relations with an exponent of β. The projectile penetrates the target after the sabot is decorticated by the shelling device. They have very elliptical (oval shaped) orbits, coming from outside Neptune towards the Sun and then going back again. The cross section of the target is a square with a side length of 600 mm and a total thickness of 800 mm. Show the class the photo of the craters on the moon, and ask them what they could be and what could have caused them. Impact Crater? In the first experiment, the students will investigate how the mass of a meteor affects the size of its crater. (2) From the shape of the impact crater, the diameter of the crater caused by the spherical projectile is close to the depth of the crater, while the diameter of the crater caused by the rod projectile (in this paper) is much larger than the depth of the crater. A device for image scanning of surface morphology was used to measure the crater size, and the scanned image and profile of the crater are shown in Figure 8. As the wave impedance of C30 concrete is close to that of granite, it is equivalent to increasing the size of the granite target. It denotes that the final crater volume increases with the increase of the kinetic energy of the projectile and the decrease of material strength [24, 25]. With the rise of hypervelocity kinetic weapons, the study of such problems began to attract more and more attention [3–5]. Experimental results of the final crater. Many craters can be seen on this image of the far side of the moon. The average diameter of the crater increases with the increase of projectile velocity. Copyright © 2020 Yanyu Qiu et al. The measured μ-values are located in the theorectical range, i.e., 1/3 < μ < 2/3. Because the tensile strength of the brittle medium is far lower than the compressive strength, the reflected tensile wave on the surface of the target will cause irregular fragmentation of the target, which is called “spalling.” If the zone of the crater caused by spalling is excluded, a bowl-shaped crater will be obtained.

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