Introduction

Cellulose comprises a major fraction in cell walls in wood and is the most abundant biopolymer. This linear polymer based on polysaccharides has excellent material properties when aggregated into hierarchical structures. The polysaccharide chains pack in crystalline and/or amorphous structures and the ratio of these depends on its origin and/or treatment. The native crystalline form is denoted ‘cellulose I’, which is a combination of two crystalline phases, Iα and Iβ, while regenerated celluloses typically contain another crystalline form denoted ‘cellulose II’. The packing of chains and the degree of crystallinity clearly influences material properties and reactivity, which are crucial properties for the development of new functional bio-based materials.

Mechanical and morphological properties correlate well with the degree of crystallinity (Kim et al. 2013; Sixta et al. 2015). Crystalline packing of cellulose chains appears to have an impact on the permeability of gases and water steam in cellulose films (Dufrense 2017) while the size of crystalline domains hampers chemical and biological reactions such as chemical hydrolysis into nanocrystalline cellulose (Klemm et al. 2011) and enzymatic degradation (Klemm et al. 2005; Park et al. 2010; Dufrense 2017). Hence it is important to estimate the degree of crystallinity for raw and modified celluloses and cellulosic materials accurately.

A few common techniques used to determine a degree of crystallinity are Wide Angle X-ray Scattering (WAXS), solid-state NMR spectroscopy and Raman spectroscopy (Evans et al. 1995; Liitiä et al. 2000, 2003; Schenzel et al. 2005; Röder et al. 2006; Park et al. 2009; Park et al. 2010; Ahvenainen et al. 2016). Depending on the method, different procedures analyzing the data have been developed. Some are straightforward and others require advanced analysis and detailed knowledge to apply them successfully. Park et al. (2010) contrasted X-ray and NMR methods on accuracy and utilization (Ahvenainen et al. 2016). Typically, peak intensity and integration routines are preferred due to their inherent simplicity while more demanding evaluation routines based on deconvolution might report values of higher accuracy. The deconvolution routine, described by Larsson et al. (1999) for cellulose I and Idström et al. (2016) for cellulose II, requires excellent signal-to-noise conditions and a 13C spectrum of soaked cellulose, which provides sharper peaks compared to dry cellulose. Both requirements together enable to build meaningful models to estimate the degree of crystallinity, which might however not be applicable to a throughput of a large number of samples.

In solid-state NMR, the experimentally important 13C T1 parameter has earlier been shown to be sensitive to amorphous and crystalline parts in polymers (Schantz 1997) and cellulosic materials (Teeäär and Lippmaa 1984, Newman and Hemmingson 1994) but requires time-consuming experiments to be used for routine work. Here, a simple and fast solid-state NMR method based on 13C T1-filter is presented. Five cellulose samples with different pre-treatment, modification, and dry content were investigated and experimentally compared to other common NMR methods and WAXS.

Materials and methods

Materials

The following five different cellulose rich samples were prepared as follows.

Microcrystalline cellulose (MCC)

Avicell PH-101, with a particle size of approximate 50 μm from Sigma-Aldrich, was used as received.

Soaked MCC (MCCwet)

MCCwet was prepared by adding 15 ml deionized water to 2 g of dry MCC. After 24 h, the excess water was decanted and the residual wet MCC was gently squeezed.

Amorphous cellulose (CellAm)

CellAm was prepared by dissolving and regenerating MCC. 2 g of MCC was added slowly to 15 ml 1-ethyl-3-methylimidazolium acetate (EMIMAc) and stirred at 50 °C overnight. The dissolved cellulose/EMIMAc mixture was poured into ethanol (50 ml) and stirred for 45 min to obtain highly amorphous cellulose (Östlund et al. 2013). The cellulose was filtered and washed with deionized water.

Sulphated nanocrystalline cellulose (CNC-SO3H)

Sulphated CNC-SO3H was prepared according to a procedure described by Hasani et al. (2008). In short, MCC was hydrolysed using 64% (wt/wt) sulfuric acid with continuous stirring at 45 °C for 2 h. The reaction was quenched by dilution with deionized water and was dialysed against deionized water, until the conductivity in the effluent remained below 5 μS. The CNC-SO3H particles were dispersed by sonication at 40% output until a colloidal suspension was achieved and then freeze dried. For further details, see the supplementary information.

2H exchanged MCC (MCCex)

1 g of dry MCC was soaked in 10 ml of D2O. The flask was sealed and let to stand at room temperature to the next day. The water was decanted off and an additional 10 ml of D2O was added, the flask was sealed and let at room temperature to the next day. The water was decanted off once again and an additional 10 ml of D2O was added, the flask was sealed and let at room temperature for 4 days. The cellulose was filtered.

The water content was calculated from the difference in weight before and after being dried in the oven at 105 °C for 20 h. MCC had a water content of 4 wt%, MCCwet of 49 wt %, CellAm of 87 wt%, CNC-SO3H of 14 wt% and MCCex 4 wt%.

Methods

Wide angle X-ray scattering (WAXS)

Wide angle X-ray scattering measurements was performed with a 0.9 mm beam diameter Rigaku 003+ high brilliance microfocus Cu-radiation source at 132 mm distance from the sample. The experimental duration was approximately 30 min. Many methods exist to quantify the degree of crystallinity, fc.x, from WAXS patterns. A regression model of 4 sharp Gaussian (crystalline) signals and one broad Gaussian (amorphous) signal with a linear baseline was applied on the WAXS patterns and an example is shown in Fig. 5. A detailed description and a review of different models and methods to estimate the degree of crystallinity on cellulose using X-ray is reported by Ahvenainen et al. (2016) and Park et al. (2010).

Nuclear magnetic resonance (NMR) spectroscopy

Solid-state NMR experiments were carried out on a Bruker Avance III 500 MHz spectrometer equipped with a 4 mm HX CP MAS probe. Experiments were recorded at a magic angle spinning (MAS) rate of 10 kHz and the temperature was set to 298 K. 1H decoupling with a “spinal64” (Fung et al. 2000) decoupling scheme at 83 kHz was applied during the acquisition. The duration of the 90° radiofrequency (rf) pulses was 3 μs for 1H and 4.2 μs for 13C. For the cross-polarization (CP) experiments, the contact time τcp was set to 1.5 ms with a 13C rf strength of 60 kHz while 1H was ramped from 45 up to 90 kHz. This ramp is designed to match both the ± 1 and the ± 2 sideband for the CP transfers at 10 kHz spinning. In combination with the contact time of 1.5 ms, the CP is very stable for small variations for example in tuning. The repetition delay was set to 2 s for all CP experiments. Saturation-recovery experiments (see Fig. 1) were recorded with a repetition time of 2 s and saturation duration of 0.5 ms using an array of 60 consecutive 90° rf pulses with a 4.2 μs delay between them. Direct polarization (DP) experiments were carried out with a 90° rf pulse and a repetition time of 400 s. 13C longitudinal relaxation time (T1) experiments based on inversion-recovery CP and a saturation-recovery scheme (see Fig. 1) were carried out with 16 delays, t, ranging from 0.1 to 400 s in a logarithmic scale.

Fig. 1
figure 1

Top: Pulse sequence schemes to estimate 13C T1 relaxation times based on an inversion-recovery with CP excitation (a) and saturation-recovery (b). The rf pulse p1 is a 90° 1H excitation pulse while p2 is a 90° 1H flip-back. For 13C, p3 is a 90° rf pulse that inverts the 13C magnetization after the CP transfer while p4 and p5 are 90°s to record the signal, which is 1H decoupled during acquisition. The saturation block is prior to the delay t. Bottom: Simulated 13C integrals as a function of t for two different T1s (black: 15 s, red: 100 s) for the inversion-recovery with CP excitation and a CP enhancement eCP of 2.5 (c) and saturation-recovery (d) experiments

The signal intensity I of the T1 experiments versus the delay t showed a double exponential behavior and was regressed using the following equation

$$ I = I_{0} \left[ {f_{\text{c}} \left( {1 - p e^{{ - t/T_{{1{\text{c}}}} }} } \right) + \left( {1 - f_{\text{c}} } \right)\left( {1 - p {\text{e}}^{{ - t/T_{{1{\text{a}}}} }} } \right)} \right] $$
(1)

to obtain T1 for the fractions of ‘rigid crystalline’, T1c, and ‘mobile amorphous’, T1a, carbon atoms in the samples. fc is the fraction of T1c and p is the pre-exponential factor, which is positive for saturation-recovery experiments. For the inversion-recovery CP experiments, p is also positive, and its magnitude is 1 + eCP, where eCP is the signal enhancement due to CP in comparison to DP. I0 is the intensity at the time t at which the signal is completely relaxed.

An NMR spectrum is composed of a number of points, which is set prior to the Fourier transform. For pseudo 2D data sets i.e. NMR spectra as a function of a delay, one might integrate the peaks of interest or use each Fourier-transformed point in the peak region to extract the integral/intensity values, which are used for fitting (see Figure S1, Supplementary information). For the saturation-recovery signal intensities, a global fit was performed for each Fourier-transformed point of a peak regions indicated in Fig. 2 using T1c and T1a as global parameters, i.e. one T1c and one T1a value was obtained for each peak region to minimize the number of fitted parameters. The peak regions are highlighted in Fig. 2. fc and p were allowed to vary, i.e. a fc and p value was estimated for each Fourier-transformed point. The obtained T1c and T1a relaxation times were used as fixed parameters to fit the inversion-recovery CP signal intensities versus t while fc and p was allowed to vary for each Fourier-transformed point. The error for the biexponential fitting routine was estimated from 100 Monte–Carlo steps.

Fig. 2
figure 2

The degree of crystallinity, fc, and the CP enhancement, eCP, for each peak region from saturation-recovery (top, red) and inversion-recovery CP T1 experiments (top, black) for MCC (a) and CNC-SO3H (b). The error was estimated from 100 Monte–Carlo steps. The fc-value of C4 for the inversion-recovery CP T1 experiment could not be estimated due to the weak signal. Assignments of the inversion-recovery CP spectra for the longest delay t were adopted from (Dick-Perez et al. 2011)

For all samples, the degree of crystallinity, fc.int, was estimated according to the traditional C4 integration method (Newman 1999) by dividing the integral of the C4 peak resonating at 86.5 to 93 ppm by the integral of the C4 region resonating at 79 to 93 ppm in the corresponding 13C CP NMR spectra. For the MCCwet sample, the degree of crystallinity, fc.dec, was estimated by deconvoluting the peaks of the C4 region according to (Larsson et al. 1999; Idström et al. 2016). Here, two new ways are presented of estimating the degrees of crystallinity, fc.inv and fc.sat, from the inversion-recovery CP and saturation-recovery experiments. The procedure is explained below.

Theoretical considerations

Dipolar 1H–13C spin interactions and 13C chemical shift anisotropy (CSA) are the main sources contributing to the 13C T1 relaxation (Ferreira et al. 2015). For cellulose if not 13C labelled under fast (> 7 kHz) magic angle spinning conditions, the magnitude of the 13C T1 relaxation time depends mainly on the dipolar interactions, which are dependent on the distance between the 1H and the 13C nucleus and the rotational correlation time τc of the 13C–1H bond (Nowacka et al. 2013).

Common methods to estimate the 13C T1 relaxation times are based on an inversion-recovery or a saturation-recovery scheme (see Fig. 1). The inversion-recovery pulse sequence inverts the 13C magnetization, which is routinely excited using a 180° direct excitation rf pulse followed by a delay, t, during which the magnetization is allowed to relax. Depending on the magnitude of the delay and on the 13C T1 relaxation time, the 90° rf pulse turns parts or all magnetization for the receiver to be detected. For the saturation recovery, an array of many rf pulses is applied during the saturation block to spoil all magnetization, which then relaxes during the next-following delay t. Therefore, the 13C integral starts negative with short delays for the inversion-recovery and at zero for the saturation recovery. The T1 can then be calculated from peak integrals or intensities recorded with various delays, t, using a single or double exponential fit (see Eq. 1).

A major drawback of recording all data points to estimate the T1 is the unreasonable long experiment durations of many days or weeks to reach a sufficiently high signal-to-noise level. As others already reported (Torchia 1978), a CP block prior to the inversion-recovery block enhances the signal-to-noise often twofold (see Fig. 1). The 1H magnetization is flipped-back after the CP magnetization transfer to allow for a 13C relaxation behavior similar to the methods without CP. However, the delay t should be 4 to 5 times of T1 to reach the plateau (see Fig. 1c, d) ensuring an accurate estimation of T1. In case of overlapping peaks and a double exponential T1 behavior, at least 16 different points needs to be recorded, which is not practical to screen when having a large number of samples.

Results and discussion

Recent 13C NMR studies based on advanced multi-dimensional magic angle spinning (MAS) experiments on uniformly 13C labeled plant cell wall and density functional theory calculations have shed light on the complexity of each broad 13C peak observed in a 13C MAS spectrum (Wang et al. 2014; Yang et al. 2017; Kang et al. 2019). It was reported that one of the C4 peaks arises from the cellulose chains on the surface of a microfibril, sC4, and the other one from the interior, iC4 (Newman and Hemmingson 1994; Wickholm et al. 1998; Wang et al. 2014; Yang et al. 2017; Kang et al. 2019). The remaining surface or interior carbons in an anhydrous glucose unit, must overlap with each other. Hence, it is less surprising that the degree of crystallinity, fc, corresponding here to the fraction of T1c, obtained from the global fit of the T1 experiments of MCC and CNC-SO3H is varying within a peak region (see Fig. 2 top for saturation recovery, red, and inversion-recovery CP, black).

13C T1 longitudinal relaxation times reflect molecular dynamics on the nanosecond time scale. As expected, and along with others (Dick-Perez et al. 2011), two distinct different T1s for each peak region were observed. The T1 of 13C atoms up to 17 s are denoted T1a and are attributed to much faster motions compared to 13C atoms with a T1c with relaxation times up to 130 s (see Table 1). Throughout the text, we will refer to T1a as the ‘amorphous’ and T1c as the ‘crystalline’ T1 although it is important to keep in mind that these relaxation times reflect the difference in mobility, often described as mobile and rigid, as does a CP spectrum and its enhancement (Nowacka et al. 2013).

Table 1 T1a,T1c and eCP obtained from global fit from the saturation-recovery experiments (see Methods and Supplementary information) for MCC and CNC-SO3H

Notably, the estimated T1a and T1c values of the different carbons for MCC and CNC-SO3H should be seen as an average of an ensemble of different morphologies. Others have reported that the T1 might be used as a measure for those (Teeäär and Lippmaa 1984; Newman and Hemmingson 1994; Larsson et al. 1997; Wickholm et al. 1998). In particular for iC4 and sC4, the T1s are merely an indicator due to the low signal-to-noise. A reliable distribution of T1s might be obtained with an excellent signal-to-noise and at least 32 variable delay times, which would take several weeks to acquire without 13C enrichment of the cellulose. The degree of crystallinity, fc, obtained from saturation-recovery T1 experiments agrees well the ones obtained from the inversion-recovery CP T1 experiments (see Fig. 2 top red and black). Unfortunately, a trustworthy fc-value of C4 for the inversion-recovery CP T1 experiment could not be obtained due to the weak signal. However, fc varied to largest extent for the peak region encompassing the C2, C3 and C5 carbons but no significant difference was found between MCC and CNC-SO3H. In comparison to MCC, CNC-SO3H showed a remarkably larger fc for C1 while fc for sC4 was found to be larger for MCC. Hence, C1 appeared more rigid in CNC-SO3H and sC4 in MCC.

The CP enhancement in comparison with DP, eCP, for 1.5 ms contact time obtained from the inversion-recovery T1 experiments, was in the range 2.0–2.2 for CNC-SO3H and 1.5–1.6 for MCC. These values agreed well with eCP values estimated from the comparison of 1D CP and DP experiments (see Table 2). The eCP values were similar for C1 and C235 for all samples but a significant difference up to 30% was found for iC4 and sC4 for MCC and CNC-SO3H (see Figure S2 for a visual examination). CNC-SO3H and soaked MCC, MCCwet, showed the largest eCP. The eCP varied significantly for the different samples (see Table 2) but less for the different carbon peak regions (see Fig. 2).

Table 2 CP signal enhancement, eCP, for five different cellulose samples estimated from CP spectra in comparison to DP spectra

The C6 region is excluded from evaluation because the CH2 group has a larger degree of freedom and is not part of the cellulose ring yielding a T1a of only a couple of seconds and a T1c between 30 and 70 s. Nevertheless, there is a difference in T1a and T1c, facilitating another relaxation filter. The difference in eCP between samples might be caused by a change in mobility on the millisecond time scale or a change of the order parameter S, the preferred orientation of the 1H–13C bond (Nowacka et al. 2013). Dick-Perez et al. (2011) reported on an order parameter of 0.8 for cellulose in the plant cell wall.

As presented in Table 1, there is a T1 difference of one order of magnitude between ‘amorphous’ and ‘crystalline’ signals of the investigated carbon peaks. Hence, a T1 filter in combination with an inversion-recovery CP to enhance signal might be used to estimate the degree of crystallinity, fc. The simulated integrals for the inversion-recovery CP method (see Fig. 1c), with an eCP of 2.5, start at I(0) = − 2.5 but end at 1 due to the similar 13C relaxation mechanism as for DP during the delay t after the 1H flip-back pulse. For a specific delay, ta0, the 13C integrals arising from the amorphous cellulose chain are at zero net magnetization while the crystalline signals, Ita0, are still negative. Since the 13C T1 of the rigid ‘crystalline’ signals are known, we can calculate the remaining negative magnitude of the rigid ‘crystalline’ signals at ta0 using

$$ m_{ta0} = 1 - p \cdot e^{{ - t_{a0} /T_{1c} }} $$
(2)

where T1c 100 s was used and p is 1 + eCP because at ta0 the second term in Eq. 1 is zero making it easy to solve for the crystallinity fc from the remaining first term. To estimate fc.inv, a 13C CP spectrum with the same number of accumulated scans is required, which comprises the total amount of signal Itot, with an experimental duration of 5 min. Hence, fc.inv is calculated as follows

$$ f_{{{\text{c}} . {\text{inv}}}} = e_{\text{CP}} /m_{{{\text{ta}}0}} \cdot I_{{{\text{ta}}0}} /I_{\text{tot}} . $$
(3)

The first part of the equation, eCP/mta0, is needed to rescale Itot to the DP scale since the signals relax to 1 in the inversion-recovery CP experiment.

A downside of the inversion-recovery CP method is that eCP needs to be estimated in order to find ta0 = − ln(1/pT1a. The eCP varies strongly with the mobility of the 13C–1H bond and its order parameter S (Nowacka et al. 2013). The eCP can be estimated by using the difference in intensity of a 13C CP experiment, the same which is used for Itot, and a 13C DP experiment with a repetition delay of at least 400 s, which is time-consuming. For accuracy, the 13C spectra require a reasonable signal-to-noise, which was obtained with 128 signal accumulations in this setup. The latter experiment took 14 h while the first one took 5 min. The experiment with the optimal ta0 took about 40 min. If the cellulose samples are similar, the eCP might only be estimated for one sample.

The degree of crystallinity, fc.sat, might also be derived from saturation-recovery experiments. For this method, a saturation-recovery experiment was needed to be recorded with a delay t of 109 s, at which the carbons from the amorphous cellulose chains were allowed to relax completely (see Fig. 1d). However, the delay t could be further optimized to save time. The degree of crystallinity is calculated as follows

$$ f_{{{\text{c}} . {\text{sat}}}} = \left\{ {1 - \left( {I_{{109{\text{s}}}} /I_{{400{\text{s}}}} } \right)} \right\} \cdot e^{{109/T_{{ 1 {\text{c}}}} }} $$
(4)

where I109s is the integral with a delay t of 109 s and I400s the corresponding value at 400 s. Although the approximation of eCP is not needed, background signals and low signal-to-noise complicate the accuracy of this method. The total experimental duration was 19 h.

In addition the 13C T1ρ was examined as a parameter, which would provide shorter experiment durations but a strong dependence on the spinlock field and very short T1ρ relaxation times complicate a meaningful implementation.

The uncertainty of fc due to missetting of T1a, T1c and eCP for both methods was simulated for given T1a, T1c and eCP (see Fig. 3). For the inversion-recovery CP method, T1a seems to be the crucial parameter while T1c and eCP have minor effect on fc. However, the accurate setting of the ta0 delay, which depends on T1a and eCP is easily judged visually. Hence the inversion-recovery CP method seems promising. If the delay would be wrong, positive 13C signals would be observed (see Fig. 4a). In contrast, the saturation-recovery method is vulnerable to very small differences in T1c and to obtain an accurate value T1c is very time-consuming.

Fig. 3
figure 3

Simulations of fc as a function of amorphous T1a, crystalline T1c and CP enhancement eCP for inversion-recovery CP method (ac) for a given eCP of 1.27, T1a 15 s and T1c of 100 s and as a function of T1c for the saturation-recovery method (d)

Fig. 4
figure 4

13C spectra of CNC-SO3H. CP spectrum with a repetition delay of 2 s (a, black) and inversion-recovery CP spectrum with a ta0 of 18.3 s (a, red). Saturation-recovery spectrum with a variable delay of 109 s (b, black) and a DP spectrum with a repetition delay of 400 s (b, red)

The 13C inversion-recovery CP signals of CNC-SO3H (see Fig. 4a, red) are negative and the CP spectrum with a repetition delay of 2 s displays positive signals (see Fig. 4a, black). The saturation-recovery spectra reveal solely positive signals with little difference in intensities for the two different delays, 109 and 400 s (see Fig. 4b, black and red). Similar spectra were obtained for the remaining samples. The saturation-recovery experiments are in general noisier due to the absent CP enhancement.

The two methods described above were applied to the five different cellulose samples and compared the results with the integration and deconvolution NMR based methods as well as WAXS. The WAXS patterns of MCC and CNC-SO3H appeared more or less identical (Fig. 5) while the CellAm pattern lack any features. The same degree of crystallinity, fc.x = 0.54, was obtained for MCCex and MCCwet. MCC had a slightly lower value of 0.52 while CNC-SO3H had the lowest with 0.48 (see Table 3). Ahvenainen et al. (2016) have shown that the estimated degree of crystallinity using WAXS is dependent on the crystallite size distribution. Hence, the lower fc.x for CNC-SO3H might be motivated by the expected smaller crystallites in CNC-SO3H. No WAXS-crystallinity analysis was performed on the alcohol coagulated amorphous cellulose since the fitting model does no longer apply. However, visual inspection of the CellAm WAXS pattern revealed a low degree of crystallinity. It should be known that cellulose crystallinity measurements from X-ray patterns can never be directly compared with NMR methods due to the crystalline size interaction and choice of analysis method affecting the final crystallinity result. However it can still be useful to do so since Avicell PH-101 is a commercial product that can be used by anyone to repeat our experiments.

Fig. 5
figure 5

Wide-angle X-ray scattering pattern for MCC, MCCwet, MCCex, CellAm and CNC-SO3H

Table 3 Estimated degree of crystallinity, fc.inv, fc.sat, fc.int, fc.dec and fc.x for five different cellulose samples

The estimated degrees of crystallinity, fc.inv, fc.sat, fc.int and fc.dec, are summarized in Table 3. Except from the amorphous cellulose sample, the lowest degree of crystallinity fc.inv was observed for the MCC and MCCex, whose labile hydroxyl hydrogens were exchanged from 1H to 2H. CNC-SO3H appeared slightly more crystalline compared to MCC and the addition of water seems to impact the crystallinity positively. There are only small variations between the different carbon atom regions.

The degree of crystallinity fc.sat obtained from saturation-recovery experiments differs significantly from fc.int except for the CNC-SO3H sample. As mentioned earlier, these spectra are noisier resulting in a larger error, while the background signal of the probe and rotor contributes to the integration. A slight difference in T1c could also explain the different results.

fc.int based on the integration method is calculated from the ratio of the two C4 signals and differs about 10% compared to fc.inv expect for MCCwet. This method works only if eCP is the same for both signals. The same is true for the deconvolution method, which gave a fc.dec of 0.56 for MCCwet. The deconvolution method works solely for wet samples as it requires sharp lineshapes.

The fc.x from the WAXS results are similar as the fc.inv except for CNC-SO3H. As mentioned earlier, one reason might be a smaller crystal size compared to the MCC samples. It should be emphasized again that WAXS uses the scattering of X-rays to estimate the degree of crystallinity while CP-based NMR methods independently on the integration, deconvolution or the presented inversion-recovery method observes a difference in mobility. Although WAXS takes only 30 min to record, the WAXS pattern must be deconvoluted. Our proposed method, if similar cellulose samples, could be applied routinely using a sample changer to measure a lot of samples.

Conclusion

By this work, a solid-state NMR method is proposed to obtain degree of crystallinity for cellulose, both native and regenerated. The method is based on 13C NMR as a mobility indicator due to the large difference in local mobility between rigid (crystalline) and mobile (amorphous) cellulose material. An inversion-recovery CP method described here allows, by applying a T1 filter, to access the degree of crystallinity after estimating the CP signal enhancement. The routine is user-friendly since only a spectral integral has to be calculated, which is fed into a simple equation and the degree of crystallinity is obtained for all carbons apart from C6. Measurement time is drastically reduced compared to contemporary solid-state NMR experiments if the CP enhancement is known and enables a high-throughput of samples if the magnet is equipped with a sample changer. The results also recommend, in agreement with the recent literature, that the integral method of the C4 peak might be used if a similar CP enhancement of all peaks is assured.