Supplemental information-v3

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Supplemental information:
Benchmark oxygen-oxygen pair-distribution function of ambient water from
x-ray diffraction measurements with a wide Q-range
Lawrie B. Skinner, Congcong Huang, Daniel Schlesinger, Lars G.M. Pettersson, Anders Nilsson , Chris J.
Benmore
Contents:
1. Sensitivity analysis of gOO(r).
2. Numerical data description.
1. Sensitivity analysis of gOO(r).
Below we demonstrate numerically the stability of 𝑔𝑂𝑂 (π‘Ÿ) for π‘Ÿ > 2 Å with respect to assumptions on
the self-scattering, intramolecular scattering and Compton scattering (CS) subtractions. For the purpose of
the stability investigation we can rearrange equation 13 in the manuscript to give
[𝑆𝑂𝑂 (𝑄) − 1] ≅ [[𝐼𝑋 (𝑄) + 𝐼𝑋𝐢𝑆 (𝑄)]
π‘šπ‘’π‘Žπ‘ 
𝐢𝑆
π‘–π‘›π‘‘π‘’π‘Ÿ (𝑄)
− πΌπ‘‘β„Žπ‘’π‘œ
(𝑄) − 𝐢(𝑄) − 4𝑓𝑂 (𝑄)𝑓𝐻 (𝑄)[𝑆𝑂𝐻
− 1]] /𝑓𝑂2 (𝑄)
where 𝐢(𝑄) is the molecular form factor, which includes self-scattering and intramolecular scattering
π‘šπ‘’π‘Žπ‘ 
contributions, [𝐼𝑋 (𝑄) + 𝐼𝑋𝐢𝑆 (𝑄)]
is the measured x-ray differential cross-section including Compton
𝐢𝑆
scattering, 𝑓𝛼 (𝑄) is the x-ray form factor of element α, and πΌπ‘‘β„Žπ‘’π‘œ
(𝑄) is the theoretical x-ray Compton
scattering curve, which is subtracted to account for the contribution present in the measurement 𝐼𝑋𝐢𝑆 (𝑄).
π‘–π‘›π‘‘π‘’π‘Ÿ (𝑄)
𝑆𝑂𝐻
is the intermolecular O-H structure factor, where the stability with respect to using different
π‘–π‘›π‘‘π‘’π‘Ÿ (𝑄)
𝑆𝑂𝐻
curves is already shown in figures 7 and 8 of the manuscript.
𝐢𝑆
In figures s1-s3 below the effects of varying 𝑓𝛼 (𝑄), 𝐢(𝑄) and πΌπ‘‘β„Žπ‘’π‘œ
(𝑄) are demonstrated. Figure s1 is the
extreme case where the intramolecular scattering has not been subtracted. Figure s2 includes in addition
the effect of not modifying the 𝑓𝛼 (𝑄) form factors (i.e. using the IAA instead of MAFF form factors).
Finally figure s3 shows the effects shown in figures s1, s2 plus the effect of using the (erroneous)
𝐢𝑆 (𝑄)
approximation πΌπ‘‘β„Žπ‘’π‘œ
is a constant.
In spite of these rather extreme approximations, as shown in figures s1-s3, the resulting errors in 𝑔𝑂𝑂 (π‘Ÿ)
are largely confined to π‘Ÿ < 2 Å, since the main effect is additive errors, which are slowly varying in Q.
An exception is the effect of neglecting the MAFF modification of the 𝑓𝑂 (𝑄). Errors in 𝑓𝑂 (𝑄) result in a
multiplicative error to 𝑆𝑂𝑂 (𝑄). However even the effect of completely neglecting to modifiy the IAA
form factors, is shown to have only a 1-3% effect on 𝑔𝑂𝑂 (π‘Ÿ) at intermolecular distances. Further the
errors caused by inaccurate subtractions are very obvious in the 𝑆𝑂𝑂 (𝑄), 𝑆𝑋 (𝑄) and 𝐼𝑋 (𝑄) functions.
Hence the accuracy of the subtractions and normalization can be checked by confirming these behave
correctly. Checks include that (1) the measured differential cross-section tends to the correct Compton
scattering level at high Q, and (2) to the correct compressibility limit at low Q, whilst (3) the resulting
𝑆𝑂𝑂 (𝑄) oscillates around 1.
In addition, the effect of the modified Lorch transform, and r < 1.1 Å oscillations to the SOO(Q) can be
seen by comparing the raw data, to the back-transform of the modified Lorch transformed data, where r <
1.1 Å has been set to zero. This comparison is shown in figure s4.
Figure s1. 𝑺𝑢𝑢 (𝑸), and π’ˆπ‘Άπ‘Ά (𝒓) generated with a direct, unmodified Fourier transform, using the Wang
C(Q) (black), and the MAFF generated C(Q) whilst completely neglecting the intramolecular terms in the
latter C(Q) (red dashed).
Figure s2. 𝑺𝑢𝑢 (𝑸), and π’ˆπ‘Άπ‘Ά (𝒓) generated with a direct, unmodified Fourier transform, using the Wang
C(Q) (black), and the IAA generated C(Q) whilst completely neglecting intramolecular terms in the latter
C(Q) (red dashed), i.e. like figure 1, but no MAFF modification has been made to the fO, fH.
Figure s3. 𝑺𝑢𝑢 (𝑸), and π’ˆπ‘Άπ‘Ά (𝒓) generated with a direct, unmodified Fourier transform using the Wang
C(Q) (black), and the IAA generated C(Q) whilst completely neglecting the intramolecular terms in the
latter C(Q), and in addition assuming Compton scattering is a Q-independent constant (red dashed), i.e.
like figure 2, but with a worst case Compton scattering subtraction.
Figure s4. Left: 𝑄[𝑆𝑂𝑂 (𝑄) − 1] functions form the raw data (red), and after back-transformation of the
modified 𝑔𝑂𝑂 (π‘Ÿ) (black line). Right: π‘Ÿ[𝑔𝑂𝑂 (π‘Ÿ) − 1] functions generated with an unmodified Fourier
transform (red) and with the variable modification fucntion, after having had the low-r set to zero (black).
i.e. The pairs of black and red lines are related by direct unmodified Fourier transform, and modified
backtransformed SOO(Q) (black) has effectively been Fourier-filtered to remove unphysical high and low
Q-freqencies.
2. Numerical data description
Included in the “Ambient_water_xray_data.txt” file is the numerical APS 𝐼𝑋 (𝑄), 𝑆𝑂𝑂 (𝑄) and 𝑔𝑂𝑂 (π‘Ÿ)
data. The 𝑆𝑂𝑂 (𝑄) has been generated using the Zeidler et al. 𝑆𝑂𝐻 (𝑄) measurement which was obtained
using oxygen isotopes and neutron diffraction (see references 33,34 of the main manuscript). The C(Q)
𝐢𝑆
molecular form factor and πΌπ‘‘β„Žπ‘’π‘œ
(𝑄), Compton scattering were taken from Wang et al. (ref. 15). The neutral
independent atom (IAA) 𝑓𝑂 (𝑄), 𝑓𝐻 (𝑄) form factors were taken from the relativistic Dirac-Fock
calculations of Su & Coppens (ref. 22), and modified for charge redistribution according to equation 4 in
the main manuscript with δ =2.0 Å-2, and π‘Žπ‘‚ , π‘Žπ» = −1, +0.5. The 𝑔𝑂𝑂 (π‘Ÿ) function given was generated
using a direct Fourier transform with the modification function described in the main manuscript.
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