Avalanche Crystallization of 4He in Aerogel · 2016. 3. 9. · New quantum phenomena may emerge at...

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Ryuji Nomura H. Matsuda, A. Ochi, R. Isozaki, and Y. Okuda Avalanche Crystallization of 4 He in Aerogel Tokyo Institute of Technology

Transcript of Avalanche Crystallization of 4He in Aerogel · 2016. 3. 9. · New quantum phenomena may emerge at...

  • Ryuji Nomura

    H. Matsuda, A. Ochi, R. Isozaki, and Y. Okuda

    Avalanche Crystallization of 4He in Aerogel

    Tokyo Institute of Technology

  • By NASA

    Aerogel: ~ 98% high porosity,

    very transparent,

    suitable for visualizing the dynamics in it.

    98% model aerogel

    By Haard

    30 nm

    3 nm

    0. Introduction

  • No viscous effect in pores.

    No release of latent heat.

    New quantum phenomena may emerge

    at very low temperatures.

    Effect of quenched disorder, which induces

    complex energy landscape, on the crystallization

    can be revealed down to absolute 0 K.

    We are interested in the dynamics of the first order phase transition in disordered media at very low temperatures.

    Why 4He?

  • Variable volume cellPlow

    Phigh

    P (

    atm

    )

    T (K)

    superfluidnormal fluid

    bcc

    hcp

    T (K)

    superfluidnormal fluid

    solid

    bcc

    hcp

    aerogel

    Crystallization at low temperatures can be investigated systematically.

    ①②

    P (

    bar

    )

    bulkaerogel

    Bulk He crystal

  • Aerogel is in a thin glass tube and has a contact

    with the bulk crystals on the upper surface.

    10mm

    8mm

    1mm

    open surface

    Porosities: 96% made by Panasonic

    98% made by Pollanen and Halperin

    at Northwestern University

  • T (K)

    superfluidnormal fluid

    solid

    1. Crystallization of 4He in aerogel by pressurization

    P (

    bar

    )

  • 170 mK 850 mK

    Crystallization in 98% aerogel

    (50 times faster replay) (100 times faster replay)

    Avalanche at low

    temperatures

    Creep at high

    temperatures

    Transition in a growth mode

  • 98%

    ■ creep

    ▲ coexist

    ● avalanche

    Dynamical phase diagram

    2.0x10-3

    1.5

    1.0

    0.5

    0.0

    press

    uriza

    tion r

    ate [

    bar/

    s]

    1.20.80.40.0

    T [K]T (K)

    pre

    ssu

    riza

    tio

    n r

    ate

    (b

    ar/

    s)

    Competition between thermal fluctuation and disorder

    Nomura et al. PRL 101, 175703 (2008)

  • 4He crystals are formed deep in the aerogel.

    Outer bulk crystal has to be melted by the stress,

    and enter the aerogel in the superfluid state.

    Mass has to be transferred for the crystallization.

    Avalanche (quantum?) Creep (thermal?)

    t

    P

    t

    P

    a b c

    d e f

    a b c

    d e f

  • Nucleation probability

    The critical overpressure was

    measured 50 times at constant

    temperature.

    Critical overpressure at which the first

    crystal appeared.

    Clear metastability:

    not instability but nucleation

    1.0

    0.8

    0.6

    0.4

    0.2

    0.480.440.400.36

    P[bar]

    200mK1K

    P1/2 P1/2

    0 1000 100t (s)

    P

    (bar)

    0 100

  • P1/2

    0.48

    0.46

    0.44

    0.42

    0.40

    P

    1/2[b

    ar]

    1.21.00.80.60.40.2

    T[K]

    T < 600 mK

    Quantum nucleation700 mK < T < 1 K

    Thermal nucleation

    T > 1 K dissipation effect

    on thermal nucleation?

    Avalanche: quantum nucleation Creep: thermal activation

    mean critical overpressure in 98% aerogel

    Avalanche Creep

    Matsuda et al. PRE (2013)

  • Power law in the avalanche size distribution in 98% aerogel

    1

    2

    4

    6

    810

    2

    4

    6

    8100

    N

    2 3 4 5 6 7 8 90.1

    2 3 4 5

    S (mm2)

    200 mK 400 mK 575 mK

    cS

    SASN exp

    = 3

    Nomura et al., JPSJ 80, 123601 (2011).

    Editors’ choice

    Self-organized

    criticality

    (SOC) in

    quantum growth

  • cS

    SASN exp

    Sc decrease as approaching the transition.

    (due to dissipation?)

    Looks like a crossover.

    Avalanche Creep

    8.03

    2'

    2.5

    2.0

    1.5

    1.0

    0.5

    0.0

    0.60.40.2

    T (K)

    0.5

    0.4

    0.3

    0.2

    0.1

    0.0

    Sc (m

    m2)

  • 2. Crystallization of 4He in aerogel on cooling

    Due to “supersolidity”?

    T (K)

    superfluidnormal fluid

    solid

    P (

    bar

    )

  • Crystallization of 4He in 96% aerogel on cooling

    100 times faster

  • b

    c

    a

    def

    completion

    Crystallization of 4He in 96% aerogel on cooling

    beginning

    Mass supply from the surrounding bulk crystals

    into aerogel is needed to grow crystal in aerogel,

    even without pressurization.

    28.4

    28.0

    27.6

    27.2

    P (

    bar)

    0.70.60.50.40.3

    T (K)

  • Crystallization rate and Pressure of bulk crystals on cooling

    Mass flowed from the surrounding

    bulk crystals into aerogel.

  • 1. What is the driving force for crystallization on cooling?

    TSSP slsl

    11

    Equilibrium crystallization pressure is temperature independent

    at low temperatures in 4He.

    Usually neglected

    2. How mass is transported in bulk 4He crystals?

    May be related to the so called “supersolidity”.

  • But, occurrence of mass flows in 4He crystal was reported by

    Hallock et al. (PRL 2008) by direct flow measurements.

    Mass flow experiment

    Original torsional oscillator experiment by Kim and Chan

    (Nature 2004) was retracted.

    Tflow = 630 mK

  • Superfluid components at a core of edge dislocation

    Path integral Monte Carlo technique

    Boninsegni et al., PRL 99, 035301 (2007)

    This issue has not been is settled, yet.

  • Crystallization diagram in aerogel on cooling

    TgrowTinitial

    Pc

    Tgrow < Tflow = 630 mK

    by Hallock

  • Summary

    Crystallization in aerogel is via creep at high T and via

    avalanche at low T by pressurization.

    Creep growth is thermal activation and avalanche growth is

    macroscopic quantum tunneling from both crystallization rate

    and nucleation probability measurements.

    Avalanche size follows a power low: Self-organized

    critical states in macroscopic quantum tunneling.

    Crystallization on cooling was observed.

    Tgrow was lower than Tflow.

    Tgrow had a anomalous pressure dependence.

    Tgrow had a anomalously wide distribution; large supercooling

    in nucleation process.

    This can be an observation of a new crystallization mode as

    “supersolidity”-assisted crystallization in pores.