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Furthermore, while many active mitigation methods have been proposed, certain classes of debris objects are amenable to mitigation campaigns employing chaser spacecraft with existing chemical and low-thrust propulsive technologies.
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Given that these objects are difficult to target and correlate, this has many implications for the space surveillance community and will allow observers to implement better search strategies for this class of debris.
An example of this class of debris is the lower stage of solid rocket boosters, such as the third stage of Ariane 4, the H10 module, usually left from European Space Agency (ESA) as space orbiting debris [6, 7].
The quantified rainfall criteria for the hazard class of debris flow create difficulties for real-time management of debris-flow hazard on the national expressway, although it is desirable to apply the probability of the possible rainfall recurrence period (Choi et al. 2015).
Considering the fact that only a very small number of the considered sites had deposit areas with volumes exceeding 2000 m3, the grading standard was modified to reflect this range, that is, the highest class of debris storage was altered from above 5000 m3 to above 2000 m3.
This class of orbiting debris is the most dangerous for aircrafts and satellites, representing a threat to manned and unmanned spacecrafts, as well as a hazard on earth because large-sized objects can reach the ground without burning up in the atmosphere.
These debris materials, deposited by the side of the river course forming cones of debris.
TREM2 has previously been reported to promote phagocyosis of apoptotic cell debris, selected classes of pathogenic bacteria, but not zymosan particles derived from the walls of Sacchoarmyces cerevisiae, Candida albicans or other types of particulate beads (Takahashi et al., 2005; N′Diaye et al., 2009).
Debris flows occurred even in areas with an E hazard class, which was initially expected to indicate a very low likelihood of debris flow.
To date, initial investigations of coarse and fine woody debris carbon stocks across classes of latitude have indicated that these carbon stocks may be related to climatic variables [ 13].
Clearing chamber of debris.
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