CEEN 341 - Lecture 17 - Time Rate of Settlement

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  • เผยแพร่เมื่อ 28 ม.ค. 2025

ความคิดเห็น • 20

  • @ahamadromen
    @ahamadromen 6 ปีที่แล้ว +1

    Thank you very much for such nicely explaining the fundamentals. Really appreciated it !!

  • @yousefbaytam6213
    @yousefbaytam6213 6 ปีที่แล้ว +1

    thank you very much sir you're actually a life saver.

  • @nicolasramirez3944
    @nicolasramirez3944 3 ปีที่แล้ว

    Thank you for these excellent lectures!

  • @JegusGrist
    @JegusGrist 6 ปีที่แล้ว

    You're very good at teaching. Thank you!

  • @farilala8480
    @farilala8480 6 ปีที่แล้ว

    Thank you so much...well explained and easy to follow. you are amazing 💓

  • @mghlakhine
    @mghlakhine 2 ปีที่แล้ว

    Thank you very much.

  • @mohammedashraf3813
    @mohammedashraf3813 5 ปีที่แล้ว

    u Are sooooo great thankkkkk you hope to make more lessons (postgraduate student in National technical University of Athens )

  • @abduljabbarkhan9107
    @abduljabbarkhan9107 4 ปีที่แล้ว

    Say, there are four layers below a square footing. Up to the depth of footing the soil is clay.
    First layer: clay soil, thickness H1, coefficient of consolidation: Cv1
    Second layer: clay soil, thickness H2, coefficient of consolidation: Cv2
    Third layer: sandy soil
    Fourth layer: clay soil, thickness H4, coefficient of consolidation: Cv4
    The fourth layer is followed by impermeable rock.
    How would you apply Terzaghi's classical formula , t = Tv/Cv*hd^2 to this problem? (hd = drainage path)
    To be more specific, how can we calculate time required for 50%
    consolidation of entire soil system? What will be the values of Cv and
    hd for the first layer?

    • @victorcaraballo5457
      @victorcaraballo5457 4 ปีที่แล้ว

      Hi. I think Hdr for the first layer has to be Hdr = Ht, because we can consider that the second layer is "impermeable" (to simplify) and first layer is single-drained. Another way to do it is consider Hdr = H1+H2 for the first layer, and find a way to get an "average" for Cv1 and Cv2 to use it for Tv equation for the first layer. That's only my opinion.
      For second and fourth layer we can consider only single-drained system, so Hdr = Ht.
      I hope you get the answer soon. That's an interesting question.

  • @aliabdulrazaq512
    @aliabdulrazaq512 6 ปีที่แล้ว

    100% amazing teaching thank you .....

  • @abduljabbarkhan9107
    @abduljabbarkhan9107 4 ปีที่แล้ว +1

    Sir, I have a situation: first layer is a clay with thickness H1 and coefficient of consolidation Cv1, the second layer is also a clay layer with thickness H2 and coefficient of consolidation Cv2, the third layer is a sand layer with thickness H3, the fourth layer is again a clay layer with thickness H4 and coefficient of consolidation Cv4. How can I apply Terzaghi's solution t = Tv/Cv*hd^2 for such situation?

  • @mehulkatakiya4892
    @mehulkatakiya4892 5 ปีที่แล้ว

    Sir, at 14:56, you are showing the area covered with a green mark on left of u(z) line, won't that area be right of u(z) line?

  • @bishoomaser
    @bishoomaser 6 ปีที่แล้ว

    Where is lecture 16 ??

  • @alxms10
    @alxms10 7 ปีที่แล้ว +4

    Hi
    Is there no Lecture 16?

  • @shahofheartz
    @shahofheartz 5 ปีที่แล้ว

    Lecture 16 and 22 Please?

  • @burakceylan9409
    @burakceylan9409 6 ปีที่แล้ว +1

    kralsın

  • @mehulkatakiya4892
    @mehulkatakiya4892 5 ปีที่แล้ว

    SIr, how OC soil can have a higher value of k than NC soil?

    • @jacksonzheng4288
      @jacksonzheng4288 5 ปีที่แล้ว +1

      if you check the consolidation curve, OC part has larger void ratio than NC part

  • @rayoaklight
    @rayoaklight 5 ปีที่แล้ว

    lecture 16 and 22 please sir