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Tidal disruption of NEAs - a case of P\v{r}\'ibram
Earth and Planetary Astrophysics · Submitted 22 Mar 2011
abstract compiled · 2026-09-23 · no language-model review
The authors' main claim The Earth's tidal forces would disintegrate a fraction of NEA population into smaller objects.
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The abstract, sentence by sentence
This work studies the dynamical evolution of a possible meteor stream along the orbit of the P\v{r}\'{i}bram meteorite, which originated in the tidal disruption of the putative rubble-pile-like parent body during a close approach to the Earth. We assumed the disruption at the time when the ascending or descending node of the parent orbit was close to the Earth's orbit. In the last 5000 years, the P\v{r}\'{i}bram orbit has crossed the Earth orbit twice. It happened about 4200 years and 3300 years ago. In both cases, we modeled the release of particles from the simplified model of rotating asteroid, and traced their individual orbital evolution to the current date. It takes several hundred years to spread released meteoroids along the entire orbit of the parent body. Even today, the stream would be relatively narrow. Considering a model parent body with physical parameters of the asteroid Itokawa, the complete disintegration of the object produced 3.8$\times10^{11}$ meteoroid particles with diameter $\geq$ 1\,cm. The meteor activity observed from the Earth is revealed and justification of follow-up observation during suggested activity of the shower in the first two weeks of April is discussed. The Earth's tidal forces would disintegrate a fraction of NEA population into smaller objects. We evaluate the upper limit of mass of disintegrated asteroids within the mean NEA lifetime and the contribution of disrupted matter to the size distribution of the NEA.
background contribution method result interpretation main claim
| # | sentence | role | the authors' own work | states the main conclusion | strength |
|---|---|---|---|---|---|
| s0 | This work studies the dynamical evolution of a possible meteor stream along the orbit of the P\v{r}\'{i}bram meteorite, which originated in the tidal disruption of the putative rubble-pile-like parent body during a close approach to the Earth. | contribution 0.99 | 0.79 | 0.20 | hedged possibility 0.91 |
| s1 | We assumed the disruption at the time when the ascending or descending node of the parent orbit was close to the Earth's orbit. | method 0.99 | 0.61 | 0.03 | asserted 0.64 |
| s2 | In the last 5000 years, the P\v{r}\'{i}bram orbit has crossed the Earth orbit twice. | result 0.74 | 0.60 | 0.05 | asserted 1.00 |
| s3 | It happened about 4200 years and 3300 years ago. | result 0.84 | 0.62 | 0.04 | asserted 1.00 |
| s4 | In both cases, we modeled the release of particles from the simplified model of rotating asteroid, and traced their individual orbital evolution to the current date. | method 0.99 | 0.94 | 0.05 | asserted 0.98 |
| s5 | It takes several hundred years to spread released meteoroids along the entire orbit of the parent body. | result 0.93 | 0.76 | 0.12 | asserted 0.99 |
| s6 | Even today, the stream would be relatively narrow. | result 0.90 | 0.82 | 0.13 | asserted 0.80 |
| s7 | Considering a model parent body with physical parameters of the asteroid Itokawa, the complete disintegration of the object produced 3.8$\times10^{11}$ meteoroid particles with diameter $\geq$ 1\,cm. | result 0.93 | 0.83 | 0.10 | asserted 0.97 |
| s8 | The meteor activity observed from the Earth is revealed and justification of follow-up observation during suggested activity of the shower in the first two weeks of April is discussed. | future work 0.62 | 0.63 | 0.11 | asserted 0.70 |
| s9 | The Earth's tidal forces would disintegrate a fraction of NEA population into smaller objects. | background 0.47 | 0.16 | 0.22 | hedged possibility 0.60 |
| s10 | We evaluate the upper limit of mass of disintegrated asteroids within the mean NEA lifetime and the contribution of disrupted matter to the size distribution of the NEA. | contribution 0.86 | 0.87 | 0.16 | asserted 0.79 |
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Original abstract
This work studies the dynamical evolution of a possible meteor stream along the orbit of the P\v{r}\'{i}bram meteorite, which originated in the tidal disruption of the putative rubble-pile-like parent body during a close approach to the Earth. We assumed the disruption at the time when the ascending or descending node of the parent orbit was close to the Earth's orbit. In the last 5000 years, the P\v{r}\'{i}bram orbit has crossed the Earth orbit twice. It happened about 4200 years and 3300 years ago. In both cases, we modeled the release of particles from the simplified model of rotating asteroid, and traced their individual orbital evolution to the current date. It takes several hundred years to spread released meteoroids along the entire orbit of the parent body. Even today, the stream would be relatively narrow. Considering a model parent body with physical parameters of the asteroid Itokawa, the complete disintegration of the object produced 3.8$\times10^{11}$ meteoroid particles with diameter $\geq$ 1\,cm. The meteor activity observed from the Earth is revealed and justification of follow-up observation during suggested activity of the shower in the first two weeks of April is discussed. The Earth's tidal forces would disintegrate a fraction of NEA population into smaller objects. We evaluate the upper limit of mass of disintegrated asteroids within the mean NEA lifetime and the contribution of disrupted matter to the size distribution of the NEA.
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According to the theory of formation and evolution of small bodies of the Solar System [ref] , meteoroid streams are formed mainly as a result of the activity of comets or the ejection of meteoroids from cometary nuclei with various initial velocities [ref] .
Statistical Equivalence of Metrics for Meteor Dynamical Association · Introduction · 0.97
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