peak overpressure vs scaled distance for tnt surface bursts (hemispherical charges)

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  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    UNCLASSIFIED

    AD NUMBER

    AD443102

    NEW LIMITATION CHANGE

    TO

    Approved for public release, distribution

    unlimited

    FROM

    Distribution: Further dissemination only

    as

    directed

    by

    allistic

    Research

    Lab.,

    Aberdeen

    Proving

    Ground,

    MD.,

    Apr

    1964

    or

    higher DoD

    authority.

    AUTHORITY

    USAARDC

    ltr, 7

    Sep

    1977

    THIS

    PAGE IS UNCLASSIFIED

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    pull,

    11II1

    f l

    --. MEMORANDUM

    REPORT NO. 1518

    "-21

    APRIL

    1964

    .71443102i

    n,

    a AV

    PEAK OVERPRESSURE

    VS SCALED

    DISTANCE

    FOR

    TNT SURFACE

    BURSTS

    (HEMISPHERICAL

    CHARGES)

    C.N.KIngery

    B. F. Pannill

    till,l

    RDr

    & EProject No.

    1MOO.5O

    !.O-5W

    "BALLISTIC

    RESEARCH

    LABORATS'I"ES

    ABEn:R:DEN PROVING RRO1ND. MARYL AND'

    "RPioducmb FCom

    Bes Avalgable

    Copi

    k7

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

    3/23

    NOTICE:

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    a

    deflnitely related

    government

    procurement

    operation,

    the, U. S.

    Government tbereby

    incurs no

    re~ionsibility,

    nor

    utiy

    obligation whatsoever; and

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    fact

    that

    tho GoverTn-

    met ayhave

    fo fOtedI ~ 4Nriehed,

    ohr~ in nn w

    supplied

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    neil

    any

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    that

    may

    in

    any

    wny

    be

    related

    thereto.

    e iy

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    DDC AVAILABILITY

    NOTICE

    Qualified

    requesters may obtain copies

    of

    this rcportl'

    from

    DDC.

    Foreign

    announcerment

    and di~semincktion

    of

    Thii-,

    ,port,

    by DDC .1

    not

    authorized.

    The

    P'

    ndings in this

    report

    arv not to

    1:.:

    con t.rwr.-t'

    no

    an

    officia) Departne.n

    of the

    Ar-nTW

    [xgzit.

    on.

    edo"00

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    (~r~1~lMWORM~UM

    RE~PORT

    NO.

    1518

    APRIL

    1964

    PE~AK

    OVERPRESSURE

    VS

    SdALED

    DISTANCE

    FOR

    TN~T

    SURFACE'

    BU1STS

    (HFaMSPHER.ICAL

    CIMA1OES)

    C. N.

    Kingery

    B. F.

    Pannill

    Terminal

    Balliatice

    Ltabora~tory

    Program

    wau

    o.uppor'ted

    in

    pr~rt by

    the

    Derenvo

    Atomic

    Support

    Agcr,,ny;

    WEB

    NO.

    02.0b)1

    Reproduced

    Fro

    Bfest

    Available

    C

    R TI

    & E

    Project No.

    IM010501A006

    A i~:~~

    I'

    l N

    I H OVILN

    G R 0U

    N

    D,

    M

    A

    R

    Y1,AN 1

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    B3A

    L LIS

    T IC

    RE SE

    A

    RC

    H L

    A

    B

    RA T

    H I

    N

    MEMORANDUM REPORT NO. 1.5,03

    CNKingary/I

    31II'lnni i i pnr1

    Aberdeen. Proving Ground, Md .

    April

    1964

    PEAK

    CV

    .PRES39RE~ VS3

    SCALED

    DIS1TANCE

    FOR~ TNT SURFACE

    13UIR M

    (HEMISPHERnICAL CHtARGES~)

    AMSTRACT

    This report

    containa a

    preaentation

    of' peak

    overprearlu~re verouui

    .:;cati

    dioutance

    va~lues derived from emnpiLrical

    mcar~urcmanti:no

    by

    Ctuinda,

    1.hr,

    United, Kingdom axid the United 3tateo.

    The can ~muflmwti3

    wcrt made, on )

    a~nd 100

    ton. TNT t3urface

    burote.

    Thc chargetit wt.rv

    hemiop~heric~al in

    :iluyt

    wid

    the

    1nrvtrumentation

    included

    overprcuoiure

    veri',i

    LIMV

    Fggr?:

    rI.d.

    Ulc 110UtAO

    optical Lihock front

    velocity technique for detti-rminin&g

    ptlLk

    ovtrp~rc~u~rt-.

    0

    0y

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    TABLE

    OF CONTENTS

    ABSTRACT .................... ......... ................... .

    OBJECTIVES

    .

    .

    BACKGROUND .

    .

    . .

    RESULTS.

    ....... . . . . . . . . . . .

    SCALING. ....... . . . .

    . . . . .

    COMPARISONS

    .....

    . ..........

    I.0

    1WREKE S

    ...

    -- 0

    0

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    JECTrVES

    The

    primary

    objective

    of this

    report

    is

    to

    present

    a

    compilation

    of

    overpressure

    measurements

    obtained

    from

    a

    aeries

    of TNT

    detonationo.

    For

    maMy

    years

    there

    has

    been

    a

    need

    for

    a

    reliable

    aurface

    burnt

    peak

    ovcrpr,3urc'

    versus

    distance

    curve

    extending

    from

    2000

    psi

    to

    .01 psi.

    Curves

    presenting

    overpressure

    versus

    radial

    distance

    (measured

    and

    theoretical)

    have

    been

    available

    for many

    years

    for

    spherical

    charges

    detonated

    in

    free

    air.

    ThI

    is

    not

    true

    however,

    for curface

    burst

    overpreosu-re

    curvez

    which

    In

    generalrn

    have

    been

    over a

    limited

    range

    of overpressure.

    and

    haed

    on

    either

    ,nial.l

    charges

    or

    charges

    fired

    utdor

    variouu

    environmental conditionn,

    making

    reliable

    scaling

    difficult.

    It

    ic

    the

    objective

    of

    thin

    report

    to

    combij,"

    measurements

    made

    by

    Canadian,

    United

    Kingdom

    and

    United

    Statet

    cn.Ltint

    into

    one

    report

    which

    might

    be

    used

    as a

    s

    tandard

    for TNT

    nurJace

    burotlt.

    BACKGROUND

    Tho

    Sufrield

    Experimental

    Station (0003)

    working

    under

    tch guLdzhtct

    oul

    the

    Defense

    Research

    Board

    of

    Canada

    begnn

    a oeriezz

    or ['Lhld

    txprtintmto

    relating

    to

    blast

    an&

    shock

    using

    yleldn

    of

    5

    tons of'

    TmpN

    n

    1959.

    phe U.2.

    was

    invited

    to

    participate

    in

    one of

    the

    trialti

    in

    J),ptemhr

    b9. W'

    accepted

    this

    invitation,

    and

    sent a

    blast

    tcaunz

    from

    the B3"Jli:slc

    ,.rienroh

    Laboratories

    (BRL)

    to

    Gntablish

    a

    blast

    line

    and to

    mnanure

    the

    overpreorurt.

    versus

    time

    at

    selected

    Airtances

    from

    ground

    zero.

    The

    preiminlrary

    reunl

    tL:

    were

    reported

    in

    a

    technical

    paper

    publirbed

    by

    01+,`

    wlth

    it very

    lUn Lt4, d

    distribution('l).

    The

    results

    obtained

    by

    the

    Canadian

    teum

    were

    reported

    Ln

    SuTield Technical

    Ppnr No. 0 along with

    renult:n of Vour

    other 5 ton

    shoto.

    The

    Car.adian

    results

    were

    prJrnarily

    peak

    overprenuiure

    vwlueo

    obtixvn'dti

    from

    5.

    hoto-optical

    technique.

    In

    1960

    a 20

    ton

    TNT

    test

    was

    conducted

    at

    SES

    i,_n,.L..

    Lvh!

    U.

    2.

    nponoored

    several

    projecto.

    One of

    the

    major

    projuetti

    fruoi

    thW U.

    ., IL

    the

    measurement

    of overpressure

    versun

    diotance

    by BP'.

    Tih

    United

    Kingdom

    (UY,)

    also

    participated

    with

    several

    eprojecto,

    one

    of

    which

    won at,,zo

    U)

    measure

    overpre,::uru

    versun

    distance.

    A

    Tripartite

    blaut

    line

    wan

    establithed

    and the

    three

    countriei

    placed

    varioui

    pr.: uuru

    tLrf f

    zzur!,

    at

    zi;mLlar

    diotaneeu

    along,

    thb-

    bl.u t

    int',v or

    cumpart:!con.

    h :

    rrzu

    lt:,

    Reproduced

    'rFo'

    Best

    Available

    CoPY

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

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    from the

    tripartita

    blast line

    were published

    in

    Suffield Report No. 203J3.

    A

    third

    test

    in

    which

    the

    BRL

    participated wan

    the 1961

    Canadian

    .1Oo

    t

    triLl. Ucre

    again

    Canada, the U. K.

    and

    the

    U.

    S.

    inotrumented

    blast lines

    and

    recorded the overpressure verouo time

    at

    LCl

    (Ctcc1htW)tc;C

    from ground

    zero. The

    results

    from

    this

    test have not been publicuhod

    in

    final

    form

    by all participants although

    preliminrvy data

    io

    avallabl.c.

    The

    final U. S.

    data

    are

    available

    in

    a

    BRL

    report and

    the

    preiLmintLry

    data from Canada

    were obtained

    from

    private correopondence 5).

    Data from

    the

    U. K.

    are reported

    in reference

    (6) and have altio

    boer compiled

    in

    thL;

    report.

    RESULTS

    The

    values

    of peak overprornure

    meartured

    by the vrarJ.ouzc

    counLriui told

    presented.

    in the referenced

    sources were till

    cnled to

    a one

    pounc ;.qutvil,,'t1

    at standard Bca-level

    conditions.

    A

    total,

    or 2'(3 (1iau.

    poirntt wtw Utwetd

    ,t

    etabl.iohing

    th. curve ao

    presented in

    Figuro

    i.

    The .ie

    point:

    W(X1, pUm;,nclw

    on

    TBM

    cardo

    "o

    ocaled

    c1iotance (%)

    vdrruo

    cc'e,-d

    ovorpre:,turc

    (P,.

    (x)

    in a nel.ed

    dirtancu and

    equaloR/W where

    R

    -

    actual

    d

    Lotatnc I(

    r,..

    and W

    u yield in pounda.

    Therefore,

    % IL equai,

    to H 'or a

    one

    poinnd 'ulia,.,

    The

    logarithmn correopinding

    to thence

    data point'

    wort,

    eomputed,

    and by i

    method

    of

    least

    aquareo the coefficients

    for

    a

    po]ynormia,

    equttrion wer,.

    derived.

    The

    recu.tt

    io:

    In 7.0452041

    -

    1.62T77561

    X - .2'(5990I.1,11

    X'

    -

    .O659731y6

    X3 + .00651il2561

    6 X

    256A

    X"

    (I)

    - .020072553

    X6

    +

    .O030.904h9

    X7 - .0001598),()i

    X"

    where

    X m log. X

    with

    X

    values

    from 0.5 to

    440.

    This equation, while

    fitting the

    pointu

    well over the

    rtuit

    of'

    vilu,-.:

    given.

    would

    be misleading if

    u3ed in

    the very low

    prc.ture

    ruglon (belo'w

    0.2

    psi).

    Therefore,

    all

    values beyond

    a

    %

    of

    io

    were

    procu:;:

    d

    throuj;i

    1.h,

    computer, atuming

    an exponential

    decay and

    the

    Following ,q!ulttti

    wa:

    derived for the low pressnure

    range.

    P

    226.61762

    %"I>

    06.591

    where

    14 C

    -c---

    l

    ft m

    C6

    -

    c%_

    PERCENT+

    PERCENT-

    PERCENT PERCENT

    1 23

    1

    20

    1

    43

    15.7

    2

    18 2 18 2

    79

    29.O

    3

    16 3

    17 -j3

    112 41.0

    1 0 4

    15 4

    137

    50.0

    5 11 5 10 5

    158

    57.8

    6

    7

    6

    6 6 171 62.5

    7

    4

    7 3

    7 178

    65.0

    8 5 8

    9 8 192

    70.2

    9

    6 9

    2 9

    200

    73. 1

    10 9 10 5

    1o 214

    78.2

    11 5 11

    5

    11 224

    82.0

    S.. 12

    4

    12 4 12 232

    85.0

    "13 6 13

    4 13

    242 C8.5

    14 0 L4

    4 14 246

    90.0

    15

    5

    15

    0 i5

    251 92.0

    16

    L 16 1 16

    253

    92.5

    17

    1

    17

    L

    L7 255

    93.5

    18 1 18

    0 18

    256

    93.6

    19

    3 19

    1 19

    260

    195.0

    20

    1

    20

    3

    20 264 96.6

    21

    0 21 2

    2L 266

    97.4

    22 0

    22

    1 22 267

    97.6

    23 0 23 2 23

    269 98.4

    24

    0 24

    1

    24 270

    98.9

    25 0 25

    1

    25 271

    99.

    26

    0

    26

    L

    26 272 9.95

    27 C 27 1

    27 273

    100.0

    . TOTAL NUMBER OF

    POINTS WAS 273

    e ,

  • 8/9/2019 PEAK OVERPRESSURE VS SCALED DISTANCE FOR TNT SURFACE BURSTS (HEMISPHERICAL CHARGES)

    16/23

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    1

    IL

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    ~

    ~

    1

    ;1

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    t

    I

    0

    ~

    f

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