Me vidéo konplè majistra Jean claude Mondesir ak tout akrolit li yo…

3 min de lecture

Okap se kon’w pran ou konnen !

Vidéo montre a klè se pawòl tafya JEAN CLAUDE MONDESIR,ak akrolit li yo tap bay yon katèl meri divize.

Nawoon Marcellus te chwazi nou nan pati ki rele boukliye pou te bloke vil la nou fèl vre. Popilasy okap la mande pou nou remèt demisyon nou rapid vit. 2 èm lindi janvier chèf kap di nou kap deside pou nou an Nawoon Marcellus prale tou ale ak li.

Jovenel Moïse ap kòde yon bò nou menm nap dekòde yon lòt bò, menm moin sa yo kitap eseye boykote 18 novanm lan nan men prezidan an. Si nou gen santiman fè sa ki po jis la demisyon demisyone. Gen moun ki komanse gen poblem sante nan vil la, nou pa konnen si se fatra santi yo ki fè sa, SANTE PIBLIK pa rache yon mo pou egzòte initil sa yo ki nan meri pou aji pou popilasyon an.

Mèsi Gérard Maxineau pou bèl interview ou te realize ak nil sa yo ki nan meri okap la, map mande [wpvideo JFgnBMj4 ] se chèf yo Nawoon Marcellus, ki mande yo aji ak moun okap konsa?

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5 réflexions sur «Me vidéo konplè majistra Jean claude Mondesir ak tout akrolit li yo…»

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    Extrusive rocks are more commonly called volcanic rocks.

    A tuff that is dominated by fragments that are larger than ash
    size is called a lapilli tuff or a welded lapilli tuff, depending on whether it’s an ash-fall tuff
    or has been welded. A different type of flow that contains large chunks of partially-cooled lava
    is called a « nuée ardente, » or glowing cloud. In a pyroclastic
    flow, fragments of tephra are kept in fluid
    suspension created by the included gases and water vapor; much like mudflows
    consist of super-dirty water. The resulting rock type is called a pyroclastic rock, from pyro for « fire » and clastic for « broken piece. » A welded tuff is a one of the pyroclastic rocks
    that forms under specific conditions.
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    Excavated rock was used to provide fill for the development of
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    The weakly welded tuffs consisted of a large amount of clastic
    material, such as glass shards and crystal fragments; the clasts were directional, and there
    were clear boundaries between them. This striking pedestrian bridge, designed by Grimshaw, spans over 320 meters and stands as an iconic structure
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    We attempted to investigate the influence of the rock formation environment on the mechanical properties of rocks, and we discuss the mechanisms of the
    differences in the mechanical properties based on the perspective of diagenesis.
    Therefore, we carried out experimental studies on the mechanical properties of tuffs with different welding degrees,
    with the integration of petrographic identification, mineral
    composition analysis, and pore structure characterization. Studying the mechanical variety of tuffs can help us figure out why,
    where, and how rockfalls occurs and effectively prevent a rockfall disaster.
    This suggests that the different mechanical properties of rock would
    influence the stability of the rock mass and, further, the rockfall volume, resulting in different disaster risk degrees.

    Rutqvist and Tsang indicated that the major reason for the variation in the
    mechanical properties of rocks was the thermal expansion of the rock from
    200 °C, and the thermal expansion coefficient depended on the temperature.

    The uniaxial compression strength and tensile strength of the strongly welded tuffs were greater than that of the weakly welded tuffs.
    The distribution of the volcanic debris inside the weakly welded
    tuffs was uneven and the cementation force was weak. The glass shards within the weakly
    welded tuffs were mostly semi-rigid. The weakly welded tuffs developed more microfractures
    internally after failure. The results of the uniaxial compression test and Brazilian splitting
    test on the welded tuffs showed that the strength of the strongly welded tuffs
    was greater than that of the weakly welded tuffs in general.

    The fracture volume of the strongly welded tuff was larger than that of the weakly welded
    tuff, and small fractures expanded into main fractures at the same
    time. Their mechanical properties (i.e., strengths) were different and with
    different failure modes. From the mineral composition and
    porosity of the two kinds of welded tuff, the weakly welded tuff and the strongly welded tuff exhibited a high consistency in the content of the quartz and feldspar.
    The CT scanning tests demonstrated the failure difference between the strongly
    welded tuff and the weakly welded tuff under uniaxial compression tests.
    There should be some microcracks in the sample that affected the development of transverse cracks.
    From the figure, it was inferred that the failure process probably started with the appearance of small axial tensile fractures inside the specimen of
    RNH01, and then a series of small tensile fractures suddenly converged
    into a shear band under the ultimate load. The presence of a multitude of tiny, fragmented clasts inside the
    fractures implied that continuous longitudinal tensional fractures occurred
    before the development of the shear fractures.

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