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1 Low-temperature thermal properties of an hyperaged geological glass Tomás Pérez-Castañeda 1 *, Rafael J Jiménez-Riobóo 2 and Miguel A Ramos 1 (1) Laboratorio de Bajas Temperaturas, Departamento de Física de la Materia Condensada, Condensed Matter Physics Center (IFIMAC) and Instituto Nicolás Cabrera, Universidad Autónoma de Madrid, E-28049 Madrid, SPAIN (2) Instituto de Ciencia de Materiales de Madrid, Consejo Superior de Investigaciones Científicas (ICMM-CSIC), E-28049 Madrid, Spain. *Corresponding author: [email protected] Abstract. We have measured the specific heat of amber from the Dominican Republic, an ancient geological glass about 20 million years old, in the low-temperature range 0.6 K ≤ T ≤ 26 K, in order to assess the effects of its natural stabilization (hyperageing) process on the low-temperature glassy properties, i.e. boson peak and two-level systems. We have also conducted Modulated Differential Scanning Calorimetry experiments to characterize the thermodynamic state of our samples. We found that calorimetric curves exhibit a huge ageing signal ΔH ≈ 5 J/g in the first upscan at the glass transition T g = 389 K, that completely disappears after heating up (rejuvenating) the sample to T = 395 K for three hours. To independently evaluate the phonon contribution to the specific heat, Brillouin spectroscopy was performed in the temperature range 80 K ≤ T ≤ 300 K. An expected increase in the Debye level was observed after rejuvenating the Dominican amber. However, no significant change was observed in the low-temperature specific heat of glassy amber after erasing its thermal history: both its boson peak (i.e., the maximum in the C p /T 3 representation) and the density of tunnelling two-level systems (i.e., the C p T contribution at the lowest temperatures) remained essentially the same. Also, a consistent analysis using the soft- potential model of our C p data and earlier thermal conductivity data found in the literature further supports our main conclusion, namely, that these glassy “anomalous”
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Low-temperature thermal properties of a hyperaged geological glass

Apr 30, 2023

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Page 1: Low-temperature thermal properties of a hyperaged geological glass

1

Low-temperature thermal properties of an hyperaged geological glass

Tomás Pérez-Castañeda1*, Rafael J Jiménez-Riobóo2 and Miguel A Ramos1

(1) Laboratorio de Bajas Temperaturas, Departamento de Física de la Materia

Condensada, Condensed Matter Physics Center (IFIMAC) and Instituto Nicolás

Cabrera, Universidad Autónoma de Madrid, E-28049 Madrid, SPAIN

(2) Instituto de Ciencia de Materiales de Madrid, Consejo Superior de

Investigaciones Científicas (ICMM-CSIC), E-28049 Madrid, Spain.

*Corresponding author: [email protected]

Abstract. We have measured the specific heat of amber from the Dominican Republic,

an ancient geological glass about 20 million years old, in the low-temperature range 0.6

K ≤ T ≤ 26 K, in order to assess the effects of its natural stabilization (hyperageing)

process on the low-temperature glassy properties, i.e. boson peak and two-level

systems. We have also conducted Modulated Differential Scanning Calorimetry

experiments to characterize the thermodynamic state of our samples. We found that

calorimetric curves exhibit a huge ageing signal ΔH ≈ 5 J/g in the first upscan at the

glass transition Tg = 389 K, that completely disappears after heating up (rejuvenating)

the sample to T = 395 K for three hours. To independently evaluate the phonon

contribution to the specific heat, Brillouin spectroscopy was performed in the

temperature range 80 K ≤ T ≤ 300 K. An expected increase in the Debye level was

observed after rejuvenating the Dominican amber. However, no significant change was

observed in the low-temperature specific heat of glassy amber after erasing its thermal

history: both its boson peak (i.e., the maximum in the Cp/T

3 representation) and the

density of tunnelling two-level systems (i.e., the Cp ∼ T contribution at the lowest

temperatures) remained essentially the same. Also, a consistent analysis using the soft-

potential model of our Cp data and earlier thermal conductivity data found in the

literature further supports our main conclusion, namely, that these glassy “anomalous”

Page 2: Low-temperature thermal properties of a hyperaged geological glass

2

properties at low temperatures remain essentially invariant after strong relaxational

processes such as hyperageing.

PACS numbers: 65.60.+a, 64.70.P-, 63.50.Lm, 81.40.Cd

1. Introduction

The search of amorphous materials with exceptional properties such as remarkable kinetic or

thermodynamic stability and high density has been the focus of much interest in recent years [1–

6]. The reason is rather obvious: not only fundamental clues are hidden behind those ideal

glasses, but there is also a potential interest for their technological applications such as

development of new pharmaceuticals or new materials for the polymer industry. Among

different possible ways to obtain these higher-quality lower-enthalpy glasses, physical vapor

deposition of organic glasses at temperatures 15−20% below their glass-transition temperature

Tg has shown up as one of the most successful techniques [1,2,5] for obtaining so-called

ultrastable glasses, with extraordinary kinetic and thermodynamic stability within the

laboratory time-scale. A controlled evaporation rate in combination with an optimal substrate

temperature have proved to drastically favour two-dimensional mobility [2] and, as a

consequence, low-energy-minima states in the potential-energy landscape [7,8] for the studied

glasses. As pointed out in [6] however, an open question is whether vapour deposition provides

access to isotropic, supercooled liquid states close to the Kauzmann temperature, or whether it

unavoidable leads to the formation of new, 2D low-energy structures that should not be viewed

as representative of the isotropic bulk liquid state.

Since the glass is always in a thermodynamic state of nonequilibrium, glasses experience

continuous structural relaxational processes below Tg, slowly leading them to lower energy

states in an energy landscape plenty of local minima −the final limit being the metastable

thermodynamic state that the supercooled liquid would have at such temperature [9]. Hence a

more traditional method to obtain and study low-enthalpy glasses has been annealing

Page 3: Low-temperature thermal properties of a hyperaged geological glass

3

(intentionally controlling the glass at a fixed stabilization temperature, for a relatively long

time), or ageing (the equivalent spontaneous process, occurring when Tg is a few tens of degrees

above room temperature).

Much work has been done in the past [9–14] to study the effects of ageing/annealing on

different glassy substances. However, the structural relaxation time increases at least

exponentially with decreasing annealing temperatures below Tg , when trying to get more stable

glasses. Therefore, human time scales seem too short for producing efficient-enough

stabilization processes in bulk glasses, compared to the accelerated ageing observed [5] in those

thin or ultrathin films of organic ultrastable glasses. In fact, it has been estimated [3] that it

would require between 103 and 109 years of isothermal ageing to acquire similar kinetic and

thermodynamic properties to those exhibited by vapour-deposited ultrastable glasses.

Nevertheless, we have identified and studied a different glassy system that is indeed a

conventional 3D bulk glass, and which has naturally aged for tens of millions of years (i.e., 1015

s) at temperatures T ∼ (Tg − 90 K). We refer to amber, the well-known geological glass.

Amber is an extraordinary material: it is a sedimentary organic product with exceptional

preservation properties, both of its own nature and of materials included inside it. These reasons

have made amber of great interest for scientists in a wide range of disciplines. From the glass-

science point-of-view, amber is a chemical glass [15], obtained as a result of the polymerization

of dienic functions and evaporation of volatile components [16]. This polymerization processes

drove the initial liquid resin into the glassy state. After that, thermal annealing below the glass

transition induced relaxation processes during millions of years, depending on the provenance.

This extremely-long natural stabilization process is what we call hyperageing. In particular, we

have studied Dominican amber, which has its origin in exudants from an extinct prehistoric

leguminous leaf tree, Hymenaea protera, and whose deposits range from 15 to 45 million years

ago [16,17].

Besides the thermodynamic and kinetic aspects of the glass transition and their related open

questions briefly mentioned above, another major controversial issue is that of the low-

Page 4: Low-temperature thermal properties of a hyperaged geological glass

4

temperature universal properties of glasses [18] associated to their peculiar low-energy

dynamics. Below 1 K, the so-called Tunnelling Model (TM) [19,20] accounted in a rather

simple way (essentially using only two free parameters: the density of tunnelling states or two-

level systems (TLS) and their coupling energy to phonons) for many of those universal low-

temperature properties of glasses [18], such as the quasi-linear temperature dependence of

specific heat, Cp ∝ T, and the quadratic dependence of the thermal conductivity, κ ∝ T 2. Above

1 K, a broad maximum in the reduced specific heat Cp/T 3 is also ubiquitously found in glasses

around 3−10 K, as well as a universal plateau in the thermal conductivity κ(T) in the same

temperature range [18]. This is nowadays associated to the so-called “boson peak” in the

reduced vibrational spectra g(ω)/ω 2, a not well understood but universal broad maximum first

observed in low-frequency Raman scattering [18] typically at frequencies ω/2π ≤ 1 THz, and

later by inelastic-neutron or inelastic-X-ray scattering techniques. Indeed, the boson peak and

related features of low-energy dynamics and low-temperature properties of glasses are currently

a matter of vivid debate and considerable controversy [21].

Although there is still no consensus about the microscopic nature and the ultimate origin of the

boson peak in glasses, we will employ for practical reasons the Soft Potential Model (SPM)

[22–28], one of the phenomenological approaches more often considered to explain the

universal properties exhibited by glasses both below and above 1 K, and that can be regarded

somehow as a generalization of the TM [19,20]. Essentially, the SPM is based upon the idea

that there exist in glasses additional (non-acoustic) quasi-local vibrations that can be modelled

by asymmetric quartic potentials [22–28], which include the double-well potentials of the TM.

The SPM has been shown [27,28] to account in a consistent way for most of these glassy

properties at low temperatures and low frequencies, at least up to the boson peak energy. More

recently, the theory of vibrational instability of weakly interacting quasi-local harmonic modes

[29,30] has lent further support to the SPM picture. Based on more general grounds, this theory

explains in a unified way the observed increasing density of tunnelling and vibrational states at

low frequencies or temperatures (predicting g(ω) ∝ ω4 and hence Cp ∝ T 5, in full agreement

Page 5: Low-temperature thermal properties of a hyperaged geological glass

5

with the SPM), also accounting for the universal appearance of a maximum (the boson peak) in

g(ω)/ω2 at slightly higher frequencies.

In this work we have studied the effects on the low-temperature specific heat of the natural and

extremely long ageing process (hyperageing) of about 20 million years, experienced by samples

of Dominican amber [17], aiming to find out whether these low-temperature glassy properties

significantly depend or not on the thermal history −and therefore could be depleted by annealing

or ageing processes−, or rather are intrinsic properties of non-crystalline solids.

Characterization of the samples around the glass transition Tg = 389 K has been performed via

Modulated Differential Scanning Calorimetry (MDSC), to check and quantify the effects of this

ageing on the enthalpy reduction. In order to bring back the stabilized amber into a conventional

(rejuvenated) glassy state, the very same amber samples were heated above Tg to erase their

thermal history, and then vitrified and measured again for comparison. We have also studied the

possible changes of the Debye-like phonon contribution to the specific heat by means of

Brillouin spectroscopy. Finally, we have used the SPM to quantitatively discuss the possible

effects of hyperageing on the low-temperature behaviour of this glass (i.e. the boson peak and

the TLS), as well as to critically compare them to earlier thermal conductivity data from the

literature [31].

2. Experimental

2.1 Samples

The samples studied in this work were Dominican amber ones about 20 million years old. By

using standard chemical analysis, the composition of the samples was found to be 78.6% C,

9.9% H and 11% O in mass, in reasonable agreement with other values found in the literature

[32], and with a nitrogen content ~0.1% and sulphur impurities below 0.2%. Mass density of the

samples was measured with a Mettler Toledo AB 265-S balance by means of the Archimedes

method, using distilled water as a fluid. The density of the pristine sample (the one used in heat-

Page 6: Low-temperature thermal properties of a hyperaged geological glass

6

capacity and Brillouin experiments) was ρ = 1.058 g/cm3 at room temperature, whereas for the

rejuvenated sample we measured ρ = 1.028 g/cm3. The rejuvenated sample was obtained after

heating the pristine one to 395 K, followed by an isothermal annealing for three hours under

vacuum conditions P ≤ 10-2 mbar. Since amber samples are heterogeneous and also present

impurities, it is important always to measure the very same sample of amber before and after

rejuvenation, so that any possible spurious contribution can be cancel out, or at least minimized.

Nevertheless, similar rejuvenation processes for other amber samples from the same batch,

always indicated that the densification produced by hyperaging is within 2.5−3 %.

Sample preparation for Modulated Differential Scanning Calorimetry (MDSC) experiments was

performed by manually milling the amber pieces in an agate mortar until a homogeneous

particle size of some tens of microns was achieved. For the low-temperature specific-heat

measurements, amber was cut into flat pieces, in order to optimize the contact area to sample

volume ratio, so that a good internal equilibrium could be achieved. Typical masses of the

samples employed were m ≈ 4 mg for MDSC and m ≈ 30 mg for low-temperature specific-heat

measurements. Brillouin measurements were performed using plan-parallel polished amber

plates typically less than 500 µm thick.

2.2 Modulated Differential Scanning Calorimetry (MDSC)

Modulated Differential Scanning Calorimetry on Dominican amber samples was performed

using a commercial TA Instruments Q100 apparatus. Standard aluminium pans of empty mass

m ≈ 20 mg were employed as sample holders, and N2 gas was used for purging the chamber and

optimizing thermal equilibrium of the sample. To calibrate the equipment, both in temperature

and enthalpy, certified indium was used. Measurements on every sample were conducted at

heating/cooling rates of ±1.5 K/min, and with modulating amplitude 1 K every 60 s, in the

temperature range 273 K ≤ T ≤ 450 K. All measurements comprise three heating and three

cooling curves, where only the corresponding specific-heat curves from the heating runs are

taken for the analysis. The three heating curves were also used either to check possible

Page 7: Low-temperature thermal properties of a hyperaged geological glass

7

differences between the first heating and the two following ones, or to test the reproducibility

among them.

2.3 Low-temperature calorimetry

Low-temperature specific-heat measurements were performed by using thermal relaxation

techniques, either the standard one or an alternative faster version developed by us [33], which

allowed an accurate determination of the specific heat of our samples in the temperature range

0.6 K ≤ T ≤ 26 K. The measurements above 2 K were performed in a double-chamber insert,

with a vacuum environment of 10 -7 mbar or better. The insert is placed in a 4He cryostat from

Cryogenic Systems, where a minimum temperature of 1.8 K is easily achieved by pumping the

cryogenic bath. For the experiments below 2 K a dilution refrigerator Oxford Instruments

MX400 was employed. Specific-heat data obtained from both experimental setups in the

intermediate temperature range overlapped each other very well.

The calorimetric cells employed in the 4He cryostat consist of a sapphire disc, on which a

thermometer (CERNOX 1030) and a heater (a commercial chip of 1 kΩ resistance at room

temperature) are glued diametrically opposed using cryogenic varnish GE7301. The value of the

resistance is determined using four-terminal wiring in the case of the thermometer, and three-

terminal wiring for the heater to account for the power dissipated in the wires. The sapphire disc

is suspended by three nylon threads in the centre of a copper ring that works as a controlled

thermal sink. On this copper ring, a Germanium sensor to monitor the temperature is

mechanically attached, and a commercial chip 50 Ω-resistance heater is glued, in order to

control the temperature of the thermal sink surrounding the calorimetric cell. A 70 μm diameter

and 20 cm long copper wire was used as dominant thermal link between the cell and the copper

ring, in order to provide typical relaxation times τ ≈ 30 s at 4.2 K. A Lakeshore 336 Controller is

used both for measuring the sample temperature and for controlling the temperature of the

Page 8: Low-temperature thermal properties of a hyperaged geological glass

8

thermal sink. A home-made current source and a Keithley 2000 voltmeter supplies the current

and monitors the voltage drop in the heater, respectively.

For the measurements below 2 K in the dilution refrigerator a similar cell is employed, but with

lower mass sensors in order to reduce the addenda contribution to the total heat capacity. A

ruthenium oxide chip with mass m ≈ 1 mg and resistance R = 1.02 kΩ at room temperature is

used as thermometer. A commercial chip with mass m ≈ 8 mg and (weakly temperature-

dependent) resistance R = 147 Ω at room temperature, is employed as heater. A 100 μm

diameter and 3 cm long manganin wire was put as thermal link in this case. Typical relaxation

times of the order of τ ≈ 15 s are achieved at 1 K. The temperature of the sample is measured

with a Lakeshore 370 AC Bridge. The power to the sample heater is applied with a Keithley

224, and the voltage drop is monitored with a Keithley 2000. The temperature of the thermal

sink is controlled using a Lakeshore 336 Controller.

2.4 Brillouin spectroscopy

High Resolution Brillouin Spectroscopy (HRBS) experiments were conducted to obtain direct

information about the propagation velocity of acoustic modes at hypersonic frequencies and

refractive index of the studied samples, and hence to assess the Debye-like phonon contribution

to the specific heat.

Polished plan-parallel slabs of amber, less than 500 µm thick, with several flat surfaces, were

placed inside a cryostat (Optistat CF from Oxford Instruments). An ITC 4 temperature

controller (Oxford Instruments) was used in the experiments, obtaining a temperature stability

of ±0.05 K. Low temperatures were achieved by using liquid nitrogen. The Brillouin

spectrometer set up was as follows: The monochromatic light source was a 2060 Beamlok

Spectra Physics Ar+ ion laser (λ0 = 514.5 nm). The scattered light was analysed using a

Sandercock-type 3+3 tandem Fabry-Pérot interferometer. No polarization analysis of the

scattered light was made. Both backscattering (180º) and right-angle 90ºA geometries were

Page 9: Low-temperature thermal properties of a hyperaged geological glass

9

simultaneously used [34], the latter allowing the observation of the (weak) transverse sound

peak. The backscattering geometry (180º) implies a refractive-index dependent acoustic wave

vector and the 90ºA scattering geometry is independent of the refractive index. The

corresponding wave vectors are:

;

0

2 4=q90A

λπ

0

n4=q i180

λπ , (1)

where λ0 stands for the laser wavelength and ni for the refractive index of the sample. The sound

propagation velocity (v) results from the combination of the Brillouin frequency shift, f, and the

corresponding acoustic wave vector:

20 v

90

90AλAf

= ; in

f

20 v

180

180λ

= (2)

In the case of absence of acoustic dispersion, for elastic isotropic media as glasses, these

velocities must be identical and thus information about the refractive index of the investigated

material can be obtained.

3. Results

3.1 Ageing and glass transition

First, MDSC experiments were performed on Dominican amber samples to study the ageing

signal and the glass transition temperature of these hyperaged, stabilized glasses. Using this

technique it was possible to separately evaluate the reversible (real) part of the specific heat,

which accounts for the thermodynamically-reversible processes, and the irreversible (imaginary)

contribution, which measures the enthalpy release around Tg and hence reflects the thermal

history undergone by the sample. Three heating curves are shown for every sample, as seen in

figure 1, to check any possible differences between the first heating and the two others, as well

as the reproducibility of second and third heating runs.

Page 10: Low-temperature thermal properties of a hyperaged geological glass

10

The pristine Dominican amber sample presented a prominent peak of ΔH ≈ 5 J/g around the

glass transition at Tg = 389 K in the specific-heat curve, as can be seen in figure 1(a). This is the

fingerprint of the very long stabilization process occurred roughly at room temperature (though

not strictly isothermal), thus far below the glass transition, for a period of time around 20

million years [16]. Interestingly, comparable values of enthalpy reduction have been found in

abovementioned vapour-deposited ultrastable glasses [2–5].

0.5 J / g·K

REJU

VENA

TED

3rd heating 2nd heating 1st heating

Tota

l Spe

cific

Hea

t

(a)

(b)

PRIS

TINE∆H = 5 J/g

280 300 320 340 360 380 400 420 440

3rd heating 2nd heating 1st heating

Temperature (K)

280 300 320 340 360 380 400 420 440 d

Crev

P /

dT (

mJ

/ g ·

K2 )

Temperature (K)

∆ Tg = 10 K

280 300 320 340 360 380 400 420 440 dCre

vP

/ dT

( m

J / g

· K2 )

Temperature (K)

Figure 1. MDSC measurements on Dominican amber for pristine (a) and rejuvenated −after 3 hours at

395 K in vacuum− (b) samples. Specific heat curves for each sample comprise three consecutive heating

upscans at a rate 1.5 K/min and modulating signal 1 K every 60 s. The scale for the specific heat per gram

is shown by a vertical bar in (b). The first heating curve (blue) for the pristine sample in (a) exhibits a

huge enthalpy release ΔH ≈ 5 J/g as a result of the dramatic ageing process. Further heating runs no

longer exhibit this feature, nor do the three curves of rejuvenated amber shown in (b). Both insets show

the derivative of the reversible part of the specific heat with temperature, for the corresponding heating

curves. A decrease in the kinetic glass-transition temperature ΔTg ≈ 10 K is found from the first to the

following heating curves for the pristine sample.

Page 11: Low-temperature thermal properties of a hyperaged geological glass

11

It is to be remarked that an exothermic feature seems to be superimposed on the big

endothermic peak at 389 K, what may be indicative of some residual curing occurring at those

temperatures, in analogy to an epoxy.

After the first heating up to 450 K, the ageing signal was completely removed, as can be seen

from the overlapping second and third heating curves of the specific heat, which correspond to

the canonical behaviour of the amber substance. The kinetic glass transition temperature has

been determined by the position of the maximum in the first derivative of the reversible specific

heat with temperature, dCrev/dT, see inset of figure 1(a). The glass transition moves towards

lower temperatures, ΔTg ≈ 10 K, after the first heating, as the resulting conventional glass is far

less kinetically stable [1,2].

In order to remove the thermal history (hyperageing) of the pristine sample (corresponding to

the first heating curve of figure 1(a)), an “anti-annealing” process was done. This process

consisted of heating up the sample to 395 K, and then isothermally annealing the sample for

three hours. The whole process was conducted under vacuum conditions P ≈ 10-2 mbar. After

this rejuvenation process, no further ageing signal is observed, as the peak in specific heat has

completely disappeared around the glass transition, even at the first heating of the sample, as

can be seen in figure 1(b). In this case, no difference between the first and the second and third

heating curves is observed, confirming that the rejuvenated sample has indeed lost its dramatic

thermal history of structural relaxation with ageing time. Comparison of dCrev/dT among the

three heating upscans show a perfect agreement in the maximum position, what implies that

their kinetic glass transition temperature is the same.

3.2 Debye level

HRBS measurements were performed to determine the phonon contribution to the low-

temperature specific heat (i.e., the Debye level) for the studied Dominican amber samples. In

figure 2(a), the longitudinal sound velocity dependence with temperature for 80 K ≤ T ≤ 300 K

is shown, where a constant shift towards lower values [vLrej

(T) − vLprs

(T)] / vLprs

(T) ≈ −3.3% is

Page 12: Low-temperature thermal properties of a hyperaged geological glass

12

clearly observed when rejuvenating the sample. A linear fit of data was employed to extrapolate

longitudinal sound velocity to 0 K. Transverse sound velocity could only be measured at room

temperature, due to the extreme weakness of its Brillouin peak, obtaining values vT prs(300 K) =

1403 ± 7 m/s for the pristine amber and vT rej (300 K) = 1320 ± 40 m/s for the rejuvenated

sample. However, Krüger et al. [35] have proposed a generalized Cauchy-like relation for

isotropic solids such as glasses or polymers, and shown that is very well fulfilled in all studied

cases. They showed that the ideal Cauchy relation c11 = 3c44 between longitudinal modulus c11

and shear modulus c44 should be replaced by a generalized Cauchy relation including an additive

term, and finally the longitudinal and transverse sound velocities are directly related at any

temperature (or even at any ageing time for polymers) by [35]

vL2 (T) = A + 3· vT

2 (T) (3)

Hence, by using eq. (3), the zero-temperature limit for the transverse sound velocity can be

obtained. For the pristine sample one gets vT prs (0 K) = 1722 m/s, and for the rejuvenated one,

vT rej (0 K) = 1667 m/s. This implies average Debye velocities vD

prs = 1926 m/s and vDrej = 1865

m/s for the pristine and rejuvenated amber, respectively.

In order to calculate the Debye coefficient, an estimation of the zero-temperature mass density

is also needed. This was done by using the Lorenz-Lorentz relation between mass density and

refractive index for a transparent medium

const

nn

=⋅+−

ρ1

11

2

2

(4)

where n stands for the refractive index and ρ for the mass density. In fact, a small variation in

the temperature dependence of the corresponding refractive indices was observed, as shown in

figure 2(b). As indicated above, we have measured mass density values at 300 K of ρprs = 1.058

g/cm3 for the pristine amber, and ρrej = 1.028 g/cm3 for the rejuvenated one. Extrapolations to 0

K of the refractive index as shown in figure 2(b), applying a linear fit to data in the temperature

Page 13: Low-temperature thermal properties of a hyperaged geological glass

13

range 80 K ≤ T ≤ 300 K, resulted in zero-temperature mass density values ρprs (0 K) = 1.090 g/cm3

and ρrej (0 K) = 1.031 g/cm3.

2600

2800

3000

3200

0 40 80 120 160 200 240 280

Pristine Rejuvenated

v L ( m

/ s

) (a)

0 40 80 120 160 200 240 2801.50

1.51

1.52

1.53

1.54

Refra

ctiv

e in

dex

Temperature (K)

(b)

λ0 = 514.5 nm

Figure 2. Temperature-dependent comparison of: (a) longitudinal speed of sound, and (b) refractive

index, using an excitation wavelength λ0 = 514.5 nm, for pristine (circles) and rejuvenated (squares)

Dominican amber. Extrapolations to 0 K using linear fits provide values: vLprs(0 K) = 3280 ± 30 m/s,

vLrej(0 K) = 3180 ± 10 m/s; n prs(0 K) = 1.538 ± 0.004, n rej(0 K) = 1.526 ± 0.002.

With all above data, one is finally able to determine the Debye phonon contribution to the low-

temperature specific heat, CDebye ≡ cD · T 3. We obtain Debye coefficients cDprs = 15.5 ± 0.8

μJ/g·K4 and cDrej = 18.0 ± 0.9 μJ/g·K4, for the pristine and rejuvenated amber, respectively. A

small but clear increase in the Debye level is thus observed after rejuvenation, as a result of

driving the substance back to a conventional, non-densified glass state. This is directly related to

the corresponding decrease in both sound velocity and mass density when thermally

rejuvenating the sample (see figure 2(a)), as a consequence of the produced softening in the

molecular lattice.

Page 14: Low-temperature thermal properties of a hyperaged geological glass

14

3.3 Effects of hyperageing on the low-temperature specific heat

Our main goal is to study the influence of deep stabilization and densification processes, due to

extremely long ageing in Dominican amber, on the universal low-temperature glassy properties.

For this purpose, low-temperature specific heat was first measured for a pristine amber sample

in the range 0.7 K ≤ T ≤ 26 K. After this, a thermal rejuvenation process as described above was

applied to the sample, and again the specific-heat curve was obtained for comparison in the

range 0.6 K ≤ T ≤ 26 K. Data are shown in figure 3, in the usual reduced Cp(T) / T 3 vs T plot.

Corresponding Debye levels, determined from the measured sound velocities and mass densities

as detailed in the previous section, are also shown in figure 3 by thick solid lines. As expected, a

modest increase in the Debye coefficient after rejuvenation is observed. The most remarkable

result is however that both Cp(T) / T 3 curves are strikingly similar, even exhibiting the same

position for the minimum, at Tmin=1.3 K, and the maximum (boson peak), at Tmax = 3.7 K, the

only difference being a small but clear decrease in the height of the boson peak after

rejuvenation.

In order to account quantitatively for any possible differences between the two samples, the

experimental data for the low-temperature specific heat are analysed and discussed in the

framework of the SPM [22–28]. For the sake of simplicity, we will only consider the most basic

version of the SPM [24–27], which does not account for the whole of the boson peak and other

glassy properties at higher temperatures, that has been however addressed in further extensions

of this model [29,30]. In the SPM, low-frequency dynamics of glasses is assumed to be

governed by the coexistence of ordinary acoustic (phonon-like) lattice vibrations and some

additional quasilocalised vibrations (usually called ‘soft modes’). The latter contribution is

described within the SPM in terms of asymmetric quartic potentials, from which the specific

heat is found to be approximately linear in temperature, Cp ~ T, for kBT << W (in the region

dominated by double-well potentials), W being the average characteristic energy of the soft

modes, whereas Cp ~ T 5 dominates at kBT > W (single-well potentials) [24–28]. Hence in the

lowest-temperature limit T < 1 K, the TLS contribution (Cp ~ T) is dominant, and the SPM

Page 15: Low-temperature thermal properties of a hyperaged geological glass

15

essentially agrees [28] with the TM [18–20]. In the typical representation Cp /T 3, this TLS

region is thus seen as an upturn at the lowest temperatures, followed with increasing

temperature by a minimum Tmin and a rapid increase Cp ~ T 5 [28] produced by the quasi-

harmonic soft-mode vibrations responsible for the lower-energy side, T < Tmax, of the boson

peak.

1 100

10

20

30

40

50

60

70

T max

= 3.

7 K

Pristine Rejuvenated

C P / T

3 ( µJ

/ g

· K4 )

Temperature (K)

CDebye pristine

CDebye rejuvenated

SPM

T min=

1.3

K

Figure 3. Cp(T) / T 3 versus T plot for pristine (circles) and rejuvenated (squares) states of the same

Dominican amber sample. Both curves exhibit the same position for the minimum, Tmin=1.3 K, and

maximum (boson peak), Tmax = 3.7 K, of Cp(T) / T 3, the only difference being a small decrease in the

height of the boson peak after rejuvenation. The corresponding Debye levels, obtained from the measured

elastic constants, are indicated by thick solid lines. As expected, a small increase in the Debye coefficient

after rejuvenation is observed. The two (almost indistinguishable between them) dashed lines are the

corresponding total SPM specific-heat curves below the boson peak, according to equation (5), obtained

as the sum of the elastoacoustically measured Debye levels for each case (thick solid lines) and the SPM

linear fits (see text).

Page 16: Low-temperature thermal properties of a hyperaged geological glass

16

Therefore, the simplest but still reasonable fit of the low-temperature specific heat of glasses is

just a quadratic polynomial fit in a Cp / T versus T 2 representation, as suggested elsewhere

[36,37]:

Cp (T) = cTLS T + cD T 3 + csm T 5 (5)

where the coefficients in equation (5) correspond to the contribution of the TLS, Debye lattice

vibrations and quasiharmonic soft modes, respectively. In order to produce meaningful

estimations of the coefficients using this fit, the temperature range to be applied must be

approximately 0 < T < 3/2 Tmin, [36,37] where Tmin is the temperature of the minimum in the

Cp/T 3 representation.

Previously, in section 3.2, we were able to determine the elastic Debye coefficient cD, which

should coincide with the corresponding coefficient obtained from calorimetric measurements

[37] by fitting data to equation (5). Indeed, the elastic and calorimetric determinations of cD are

found to be equal in our samples within experimental error. Nonetheless, since we have a

model-independent elastic determination of the cubic Debye coefficient cD, we will better

employ the procedure followed in [38] for butanol glasses and conduct the SPM analysis with

only two fitting parameters, cTLS and csm. In brief, one fixes the elastoacoustically measured cD

coefficient for each glass, and the excess specific heat is directly manifested after subtraction of

the corresponding cubic Debye contribution CDebye = cD T 3, by plotting (Cp−CDebye)/T vs T

4 in

order to obtain the missing T and T

5 coefficients of the SPM from simple straight-linear fits, as

shown in figure 4 and Table 1. Despite the larger data scatter due to the very sensitive chosen

axes, the expected linear behaviour is observed indeed below 2 K, what supports the validity of

the made SPM assumptions and analysis. In addition, we also show in the Cp/T 3 representation

in figure 3 the total SPM specific heat (dashed lines) below the boson peak, for the amber glass

in both cases, that is the sum of the elastoacoustically measured Debye contribution for each

glass (thick solid lines) and the SPM fitted contributions from figure 4, according to equation

(5).

Page 17: Low-temperature thermal properties of a hyperaged geological glass

17

0 2 4 6 8 10 12 140

20

40

60

80

100

(CP-

C Deby

e) / T

( µJ

/ g

· K2 )

T 4 (K4)

Pristine Rejuvenated

Figure 4. (Cp – CDebye)/T versus T

4 plot for pristine (circles) and rejuvenated (squares) Dominican amber,

in the low temperature range. A least-squares linear fit to the SPM is done (dashed lines) to obtain the

SPM parameters cTLS and csm. Fitting curves are (Cp – CDebye)/T = 14.7 μJ/g·K2 + 5.7 μJ/g·K6·T 4 for the

pristine amber and (Cp – CDebye)/T = 13.8 μJ/g·K2 + 5.1 μJ/g·K6·T 4 for the rejuvenated one. The observed

linear behaviour in the temperature range 0 K ≤ T ≤ 1.95 K supports the validity of the SPM assumptions.

Table 1. Comparison of the low-temperature parameters for the Dominican amber samples, both pristine

and rejuvenated. ρ(0 K): zero-temperature mass-density extrapolation using equation (3); vD: Debye

averaged velocity; cD: Debye phonon contribution to the specific heat determined from HRBS; Tmin, Tmax:

respective temperatures where the minimum and the maximum in Cp/T 3 occur; cTLS, csm: TLS (∝T) and

soft modes (∝T

5) coefficients of the specific heat calculated from the linear fits in figure 4 with the SPM.

Amber

glass

ρ(0 K)

(g/cm3)

vD

(m/s)

cD

(μJ/g·K4)

Tmin

(K)

Tmax

(K)

cTLS

(μJ/g·K2)

csm

(μJ/g·K6)

Pristine 1.090 1926 15.5 1.3 3.7 14.7 5.7

Rejuvenated 1.031 1865 18.0 1.3 3.7 13.8 5.1

Page 18: Low-temperature thermal properties of a hyperaged geological glass

18

From both figures 3 and 4, it is very clear that the highly densified, hyperaged amber retains all

glassy excitations at low temperatures (i.e. TLS and “boson-peak” soft modes), even

quantitatively. They appear in our case to be even slightly above those of the canonical,

rejuvenated amber, what is certainly striking.

Finally, we will make use of this SPM analysis of the low-temperature specific heat to

concurrently address and discuss earlier thermal-conductivity measurements at low

temperatures, also conducted in Dominican amber by Love and Anderson [31]. In figure 5, we

depict their thermal-conductivity data κ (T) [31] for pristine (as received) and rejuvenated (at

370 K) Dominican amber samples. Although their samples and ours could be somewhat

different (indeed, their reported glass-transition temperature is lower than that of our samples),

the thermal conductivity of glasses is not very much sensitive to material parameters [19,20]

and a joint analysis can be done. As it has been discussed in detail [27,28], the SPM main

parameter W/kB marks the crossover temperature below which the TLS dominate the low-energy

glassy dynamics and above which quasilocalised soft modes (eventually piling up at the boson

peak) do. To be more precise, this crossover is seen in the specific heat as the minimum Tmin in

Cp/T 3 (with W/kB ≈ 1.6 Tmin analytically [24], although also W/kB

≈ 1.8 Tmin was postulated from

some numerical calculations [28,39]), and in the thermal conductivity as a bend from the

quadratic temperature dependence at the lowest temperatures to the plateau region, hence as a

maximum Tmax,κ in κ/T (with W ≈ 1.6 Tmax,κ) [27]. Therefore, the main qualitative prediction of

the SPM is that the minimum Tmin in Cp/T 3 and the maximum Tmax,κ of κ/T should occur [27] at

(almost) the same temperature. The inset in figure 5 shows that for the pristine Dominican

amber one has Tmax,κ = 1.3 K (hence W = 2.1 K), which nicely agrees with our minimum Tmin =

1.3 K in Cp/T 3. Furthermore, it can also be seen in figure 5 that the thermal conductivity for the

rejuvenated amber (unfortunately not provided [31] in the whole temperature range) is again

very similar to that of the pristine sample. This supports our statement that the hyperaged glass

fully retains the universal glassy properties at low temperatures, which are not depleted by this

dramatic structural and thermodynamic relaxation.

Page 19: Low-temperature thermal properties of a hyperaged geological glass

19

0.01 0.1 1 10

10-4

10-3

10-2

10-1

κ (W

/m·K

)

T (K)

as receivedrejuvenated 370 K

SPM

0.01 0.1 1 100.00

0.01

0.02

κ/T

(W/m

·K2 )

T (K)

(= 1.3 K)Tmax

Figure 5. Thermal conductivity κ data versus temperature in a double logarithmic scale, measured by

Love and Anderson [31] for other pristine (as received) and rejuvenated (at 370 K) Dominican amber

samples. The inset shows the same data plotted as κ/T vs T, following the SPM method [27,28] to

determine a maximum Tmax,κ of κ/T and hence the basic SPM parameter W ≈ 1.6 Tmax,κ, which marks the

crossover from the TLS-dominated region (κ ∝ T 2) to the soft-mode one (plateau).The solid line is the

SPM [27,28] predicted curve for the fitted W.

4. Discussion

As briefly reminded in the Introduction, the two most characteristic types of “anomalous” low-

energy excitations in glasses and disordered solids, which pervade all their physical properties

at low temperatures and frequencies, are: (i) TLS (or tunnelling) states, and (ii) low-frequency

vibrations producing the “boson peak”. The former are well accepted to exist and account for

thermal, acoustic and dielectric glassy properties at temperatures below 1 K and energies below

1 meV, following the Tunnelling Model, though a full microscopic understanding is still lacking

[40]. The very nature of the latter is nowadays a vivid matter of debate and controversy, and

many theories and models [29,30,41–46] compete to explain low-frequency dynamics of glasses

featured by the boson peak. Furthermore, during the last forty years many different attempts

Page 20: Low-temperature thermal properties of a hyperaged geological glass

20

have been made (with unclear conclusions [47–52]) to know whether these low-temperature

glassy properties significantly depend or not on the impurities and the thermal history, and

therefore could be depleted by annealing or ageing processes, or rather are essential and

intrinsic properties of non-crystalline solids. Alternatively, some inelastic neutron-scattering

experiments in a mineral hyperquenched glass [53], seemed to point out that the boson peak is

greatly enhanced in the hyperquenched glass over that of the standard and the annealed glass.

The same trend was found in computer simulations of binary mixtures [6,41], where the

observed total maximum in g(ω)/ω

2 was found to decrease and shift to higher frequencies with

slower cooling rates.

Very recently, a much debated issue is whether or not the boson peak scales with the Debye

frequency and hence with the elastic medium constants, where again opposite views have been

published: in some cases, the Debye-reduced vibrational density of states plotted versus the

Debye-reduced frequency merge into a master curve, either when comparing hyperquenched to

annealed glasses [54], or measuring at different temperatures [55], or even during

polymerization of a reactive mixture [56], whereas in other cases [38,57,58] this scaling has

been found to fail. Moreover, some authors [59] have claimed that the boson peak in glasses is

the counterpart of the acoustic van Hove singularity in crystals, shifted to lower energy by

force-constants disorder. Then, similar to the transverse acoustic singularity in crystals, the

boson peak originates from the piling up of the acoustic states near the boundary of the pseudo-

Brillouin-zone.

The first key question is then: do excess glassy properties (i.e. TLS and the boson peak) strongly

depend on the thermal history of the glass, and hence on the reached excess enthalpy, and

eventually would disappear for ideal, extremely annealed or stabilized glasses, or rather are they

intrinsic properties of the glassy, non-crystalline state? Our findings in the extreme case of an

hyperaged geological glass, which retains −if not enhances− both its boson peak and its density

of TLS at low temperatures, undoubtedly state that these universal low-temperature glassy

Page 21: Low-temperature thermal properties of a hyperaged geological glass

21

excitations are robust against the thermal history, and intrinsic to the non-crystalline lattice. The

SPM analysis conducted to quantitatively assess those low-temperature glassy excitations in the

specific heat, as well as earlier thermal-conductivity data, further support our conclusion.

Such a clear statement cannot be made in relation to the Debye scaling, since both the Debye

level and the observed Cp/T3 boson peak do not vary strongly after the thermal rejuvenation.

Still, the slightly lower boson peak observed after rejuvenation, whereas the Debye level has

increased around 15%, points out that a Debye scaling of the boson peak is not fulfilled. One

may speculate that the unexpected decrease of the boson-peak height with thermal rejuvenation

could be related to some residual curing happening around 390 K, as said in section 3.1. The

fact that almost every physical property remains constant or behaves in the opposite direction,

suggests that its influence, if any, is not significant.

The remarkable enthalpy reduction observed in our MDSC characterization experiments, ΔH ≈

5 J/g, is comparable to those found in ultrastable thin film glasses [1–5] obtained by physical

vapour deposition, and provides further evidence that the expected huge structural relaxation

has indeed occurred in our pristine amber samples, and that our results are meaningful.

The modest but clear variations earlier found [47–52] in the low-temperature specific heat of

some glasses with different thermal history could be attributed, in our view, to the concurrent

variation of the elastic constants and the Debye contribution below the boson peak, which in

most cases were not measured. As a matter of fact, in the case of pure and dry B2O3 glass, very

different maxima in Cp/T3 for different thermal treatments were found to collapse in a single

curve after their corresponding Debye levels were subtracted [51].

Finally, during the writing of this paper, we became aware of a forthcoming publication by

Zhao et al. [60], who have investigated the dynamics of similar 20 million year old Dominican

amber via stress relaxation experiments above and below the glass-transition temperature.

Among other results, by fitting the relaxation time curve in the equilibrium liquid state to the

Vogel-Tamman-Fulcher function, they obtained a dynamic fragility index of m = 90. It is worth

Page 22: Low-temperature thermal properties of a hyperaged geological glass

22

emphasizing that Sokolov et al. [61,62] found, after analysing thirteen glass-forming

substances, that the relative weight of vibrational over relaxational excitations (i.e. the boson

peak) is larger for stronger than for fragile glass formers, in the well-known Angell’s

classification. One of the ways used by them to assess this relative weight was through the ratio

R of Debye-reduced specific-heat data at Tmin over that at Tmax, R = (Cp/T 3)min / (Cp/T

3)max. For

glass formers so fragile as to have m ∼ 90 (e.g. o-terphenyl or CKN), R was as large as 1, that is

a very shallow boson peak, whereas strong glass formers (low m indices) exhibited strong and

well-defined boson peaks, with R below 0.5. The boson peak of our pristine amber sample gives

R ≈ 0.52, which lies between the values of strong glass formers B2O3 and sodium-oxide silica,

with m ∼ 40. Therefore, amber does not follow the proposed correlation [61,62], its liquid being

dynamically fragile but its glass showing a strong vibrational boson peak.

5. Conclusions

We have studied the effects of the extremely long ageing process (an estimated period of time

between 15 and 45 million years) naturally occurred in Dominican amber, on the universal low-

temperature properties of this geological glass. With such an aim, we have measured the

specific heat at low temperatures of the same sample before and after a thermal rejuvenation

process to erase its dramatic thermal history. MDSC experiments confirmed the very large

enthalpy reduction geologically occurred in the pristine sample, in comparison to the

rejuvenated one. Brillouin-scattering experiments allowed us to determine both temperature-

dependent (longitudinal and transverse) sound velocities and refractive indices, and hence the

elastic Debye contributions to the specific heat needed to make a thorough analysis of the low-

temperature glassy excitations.

Somewhat strikingly, we have found that the pristine, hyperaged amber exhibits a strong boson

peak and a high density of tunnelling states, as high (if not even higher) as those of the

rejuvenated sample. Given the extreme structural and thermodynamic relaxation produced in

Page 23: Low-temperature thermal properties of a hyperaged geological glass

23

this glass prior to its rejuvenation, our observations should be robust enough as to reach a high

level of generality. The main conclusion is that the ubiquitous glassy excitations at low

frequencies or temperatures (TLS and the boson peak) are intrinsic to the non-crystalline state

and they are not depleted by long annealing or structural relaxation processes. These can

however influence the Debye-like elastic properties, and hence indirectly the total heat capacity.

Our results in this paradigmatic geological glass are also at odds with the previously proposed

Debye scaling of the boson peak and the correlation of the latter with the inverse of the fragility

index.

In order to test the reproducibility and general character of the presented results, similar

experiments on other amber glasses from different sources (i.e. with different chemical and

thermal histories) are currently underway.

Acknowledgements

The Laboratorio de Bajas Temperaturas (LBT-UAM) is an Associated Unit with the ICMM-

CSIC. This work was partially supported by the Spanish MINECO (FIS2011-23488 project, and

Consolider Ingenio Molecular Nanoscience CSD2007-00010 program) and by the Comunidad

de Madrid through program Nanobiomagnet (S2009/MAT-1726). T. P.-C. acknowledges

financial support from the Spanish Ministry of Education through FPU grant AP2008-00030 for

his PhD thesis. María José de la Mata is gratefully acknowledged for her technical support and

kind advice with MDSC measurements conducted at SIdI−UAM. M.A.R. is grateful to Greg

McKenna for sending us their article [60] prior to its publication.

Page 24: Low-temperature thermal properties of a hyperaged geological glass

24

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