W. Trent
Franks‡
ab,
Jacqueline
Tognetti‡
ab and
Józef R.
Lewandowski
*a
aDepartment of Chemistry, University of Warwick, Coventry CV4 7AL, UK. E-mail: J.R.Lewandowski@warwick.ac.uk
bDepartment of Physics, University of Warwick, Coventry CV4 7AL, UK
First published on 12th October 2022
Spin–lattice relaxation rate (R1) measurements are commonly used to characterize protein dynamics. However, the time needed to collect the data can be quite long due to long relaxation times of the low-gamma nuclei, especially in the solid state. We present a method to collect backbone heavy atom relaxation data by nesting the collection of datasets in the solid state. This method results in a factor of 2 to 2.5 times faster data acquisition for backbone R1 relaxation data for the 13C and 15N sites of proteins.
Longitudinal relaxation rates (R1 = 1/T1)6 report on motions with correlation times in the order of ps–ns. In the solid state, backbone 13C and 15N nuclei are typically characterized by long T1 times in the order of tens of seconds. It is common to measure the relaxation in biological systems using pseudo-3D experiments6–10 in which site resolution is achieved from a 2D correlation spectrum, and the relaxation is encoded in the third, pseudo-dimension. The delays in this third pseudo-dimension are dictated by the length of T1s, which renders the experiments for probing backbone relaxation very long.
There have been several approaches to speed up the direct collection of R1 relaxation data, usually by partitioning the signal so that only one scan is needed. Single scan methods to measure T1 were first demonstrated by Kaptein et al.11 and later adapted using magnetic resonance imaging techniques (MRI).12–14 These techniques need very sensitive samples with detection on 1H or on hyperpolarized nuclei15 such as 13C or 15N. The high sensitivity is required due to signal splitting, along with good chemical shift resolution for site resolution and powerful gradients, which are all uncommon in biological NMR, and especially so for MAS experiments. Other approaches focus on speeding up acquisition by recording several experiments at once (PANACEA,16 DUMAS17), utilizing orphaned polarization,18 encoding multiple pathways into the same experiment,19 using multiple detectors,20–22 and by interleaving experiments into the recovery delay of another.23
We recently introduced experiments to collect protein backbone 13C′ and amide 15N relaxation data with a single excitation and sequential acquisitions.24 Our previous work presented simultaneous cross polarization (SIM-CP)25 and staggered acquisitions to encode carbon and nitrogen relaxation experiments using a shared time period. The 13C′ and 15N R1 rates are collected in the time it would normally take for the 15N R1 experiment. Here we present a method to acquire R1 relaxation measurements on three nuclei of the peptide plane 13Cα, 13C′ and 15N through nested experiments, with no sensitivity loss, in the time normally required to acquire just a 15N R1 experiment.
The nutation frequencies were calibrated for 1H at 2 μs (ν1 = 125 kHz), 13C at 2.5 μs (ν1 = 100 kHz) and 15N at 4.15 μs (ν1 = 60 kHz). Heteronuclear 1H decoupling (≈10 kHz WALTZ-64)29 was applied during 13C and 15N t1 evolution and during the COSY-based transfer. 13C heteronuclear decoupling (≈10 kHz WALTZ-64) was applied during the acquisition of both 13C experiments, while 15N heteronuclear decoupling (≈10 kHz WALTZ-64) was used only for the HN acquisition. The MISSISSIPPI30 solvent suppression scheme was applied with a spinlock field of ≈50 kHz for four 10 ms intervals after the excitation and chemical shift encoding period (i.e. immediately after storing the polarization along the z-axis) and for four 20 ms intervals immediately before transfer back to the 1H for detection for each individual R1 experiment. Cross-polarization (CP) was used for the initial excitation of 13C and 15N and the transfer back to 1H for acquisition. For all the experiments the average 1H field was chosen at ≈130 kHz with a linear 15% ramp (85–100%, from ≈121.5 to 139.5 kHz) and a zero-quantum (ZQ) match condition transfer was used on 13C and 15N channel. Each 13C and 15N frequency was irradiated at a field of ≈30 kHz and the carrier placed on the appropriate resonance. The contact times were optimized individually for the 1H–X/Y CP. The CP contact times were 1.2 ms, 2.1 ms and 2 ms for 13Cali, 13C′ and 15N respectively, while they were 150 μs for the one-bond 13Cali–1H transfer and 500 μs for 15N–1H CP. Gaussian Q3 cascade pulses were used for the selective 13C inversion where a 320 μs pulse gives a bandwidth of 10.5 kHz (≈60 ppm) and 760 μs gives a bandwidth of 5.3 kHz (≈30 ppm) for 13C′ and 13Cα respectively. For the selective 13C′–13Cα coherence transfer, the J-coupling delay was 4.25 ms when 13C′ is along the transverse plane and 3 ms when 13Cα is transverse.
The program used for arranging the experiments in the Slice & Dice experiments of the R1 was created in Python 3.7. The minimum and maximum relaxation times and the desired number of points for each sub-experiment can be entered manually or spaced automatically where the Fibonacci sequence is the basis for the spacing between time points. The pulse sequences, datasets, lists, compound pulse lists, and pulse shapes can be found online on Zenodo (https://doi.org/10.5281/zenodo.5965022). The relaxation delays used in the presented experiments are given in Table S1 (ESI†). To allow for direct comparison of the relaxation rates, the same number of increments in the indirect dimension were considered for all spectra. All spectra were processed in Bruker Topspin 3.6.1 with −40 Hz LB in the direct dimension and Lorentzian to Gaussian line broadening with −20 Hz and an offset of 0.1 in the indirect dimensions. Peak assignment and integration were performed using CARA version 1.9.1.7. The integrated intensities of each well-resolved peak were normalized and fit to a single exponential to find the relaxation rate. All relaxation rates are reported at the 95% confidence level from 2000 steps of Monte Carlo error analysis.31
Measurement of relaxation rates for different types of nuclei aids obtaining a more accurate view of protein motions. In this context one could measure the amide 15N, carbonyl 13C′, alpha carbon 13Cα and, if possible, the sidechain aliphatic carbons 13Calis. The experiment time could be optimized by including the spin–lattice relaxation measurements on 13Cα and 13C′ with 15N R1s in an experiment we refer to as Slice & Dice. The magnetization transfer pathway for each nucleus 15N, 13C′ and 13Cα is illustrated in Fig. 1(a). The individual experiments are sliced into separate periods for excitation (square) and acquisition (triangle), as in Fig. 1(b). The excitation portion of the experiment has an initial CP, the chemical shift evolution and a storage pulse (Fig. S1, ESI†). With the use of a standard CP, where polarization is transferred to one type of nuclei, instead of a SIM-CP (where polarization is transferred to two types of nuclei), the excitation portion is treated separately for all the nuclei during the Slice & Dice construction. The acquisition portion of the experiment re-excites the stored polarization and then transfers it to the expected detection nucleus. The division of the pulse sequences into different blocks (indicated with squares and triangles) allows us to assemble them in the most convenient way to fit into the relaxation measurements as described below. In order to embed the blocks, we will only consider placing whole “inner” experiments into the relaxation delay of an “outer” experiment (Fig. 1). Generally, the 15N experiment requires the longest maximum relaxation delay, and the aliphatic carbons the shortest relaxation delay, so the 15N block will be made to be the first “outer” experiment, and the two 13C experiments will be the first “inner” experiments (Fig. 1(c)). The nitrogen relaxation measurement is the “outer” experiment for as long as the carbon “inner” experiments will fit into its relaxation delay. The “inner” and “outer” experiments are then exchanged when the long relaxation times of 13C are suitable to accommodate the short relaxation times of 15N that are now the “inner” experiment (as in Fig. 1(d)). In order to efficiently fit the experiments into one another, the order of the relaxation delays can be changed. It is usually possible to find a solution in which all or most of the desired relaxation times embed into one another nicely by hand, but can be a time-consuming puzzle, so a Python program was written to facilitate the creation of the experiments (see Data availability). The program will embed the experiments taking into account for the “AQ” time which includes recovery delay, excitation and evolution, 2× saturation and acquisition, and the “wait” time which ensures a minimum time between acquisitions.
The result of the ordering is an experiment similar to the one found in Fig. 1(e). There are 7 separate 13C experiments during the first 15N relaxation measurement, and then 2 and 1 in the relaxation delay of the next two 15N experiments. Then there are two 13C′ “outer” experiments with 1 and 2 15N experiments embedded respectively. The provided Python program is used to estimate the timings for these experiments. To compare the experiment times, the time is estimated on the relaxation delay list without accounting for second chemical shift dimensions or for the repetitions needed for the phase cycle, then assuming that each experiment requires the same number of scans in total. For example, for crystalline GB1, considering an “AQ” time of 2.6 s, a “wait” time of 1.5 s, and the three delay lists in Table S1 (ESI†) the Python pulse program calculated that acquiring one transient for all these datasets in the traditional way would take 157.1 s for the 15N dataset, 62.7 s for the 13Cα, and 101.2 s for the 13C′, or 321.0 s total, while it only takes 181.3 s for the embedded experiment. With the same delay list per nucleus between the usual implementation and Slice & Dice, and involving 16 transients and 64 indirect increments, the standard measurements would be 3 days and 8 hours (∼41 hours for 15N, ∼14 hours for 13Cα and ∼25 hours for 13C′), while the experimental time for Slice & Dice was ∼2 days and 2 hours.
Three sets of spin–lattice relaxation measurements for 15N, 13C′ and 13Cα are then acquired in approximately half the time necessary to collect the full complement of standard R1s, and if compared to the sole 15N standard experiment it takes only 8 h more. Alternatively, a standard 13Cα and a SIM-CP N + C′ experiment can be acquired separately. In this case, the Slice & Dice implementation takes 20% less time to collect. Further, the SIM-CP experiments suffer from ≈10% lower sensitivity while the interleaved experiments experience no loss since the Slice & Dice employs a standard CP for all of the 1H–X/Y transfer (Fig. S2, ESI†). It was found to be necessary to add a short “MISSISSIPPI” saturation period at the end of the excitation periods to ensure that the initial 1H polarization is consistent amongst all possible combinations of experiments and relaxation times.
To test our experiments we used a fully protonated uniformly [13C,15N] enriched crystalline GB1 sample. In solid-state NMR the presence of spin diffusion alters the R1 rates, losing their site-specific nature due to averaging of nearby sites. In uniformly [1H,13C,15N] labelled samples at MAS > 20 kHz it is possible to obtain site specific rates on 15N,32,33 while spinning rates > 60 kHz are required for 13C′ R1s.3,6 All our experiments were carried out on a 700 MHz 1H Larmor frequency and a spinning frequency of 100 kHz. 100 kHz MAS guarantees truncation of proton driven spin diffusion on 13Cα of protonated uniformly labelled sample,34 which allows for the interpretation of R1 measurements at these sites. At lower spinning frequencies custom labelling schemes are required to minimize the relaxation rates averaging effects of the spin diffusion.35 Further, the fast MAS preserves the site-specificity bearing an improved 1H detected spectra resolution. The R1 measurements for 15N, 13C′ and 13Cα obtained with a single interleaved experiment are here compared with the rates recorded with the following separate acquisitions: 15N (Fig. 2(a)), 13C′ (Fig. 2(b)), and 13Cα (Fig. 2(c)), where the whole assignment can be found in ESI† (Fig. S3 (13C′, 15N) and S4 (13Cα)). The rates are the same within measurement error to the standard implementation (see Fig. S7–S9 for correlation plots for the rates). The 13Cα measurement was set up to accommodate the acquisition of the aliphatic 13C, indeed the carbon dimension is folded at ≈43 ppm to divide the 13Cα resonances from the rest of the aliphatic carbons (Fig. S4 and S5, ESI†). The complete 13Cali indirect dimension is incidentally acquired during the collection of the 13Cα measurements obtaining a well resolved sidechain 1H detected spectrum which may be feasible for relaxation measurements. However, 100 kHz MAS is still often not sufficient to fully average out spin diffusion on 13Cali on an uniformly [1H,13C,15N] labelled sample34 and alternate 13C-labelling should be applied to minimise the effect of spin diffusion. For completeness, the comparisons between standard and Slice & Dice aliphatic 13C, 13Cβ to 13Cα, spin–lattice relaxation rates are reported in Fig. S6 (ESI†).
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Fig. 2 A comparison of the R1 rates for (a) 15N, (b) 13C′, (c) 13Cα obtained from the separated single-acquisition experiment (full-blue circle) and Slice & Dice (full-red triangle) as a function of the residue number. Errors bars represent two standard deviations within the correspondent rate. The shaded areas in panels (a)–(c) outline secondary structure elements in GB1 as indicated with cartoons above the panel (a). For the severely overlapping peaks, values are not included (see ESI†). |
One of the challenges for these experiments is that the sampling of the indirect dimensions is linked to one another. The spectral width needed for the aliphatic 13C, or even the 13Cα, is two to four times that needed for the 13C′ or 15N, depending on how the spectrum is folded. This discrepancy creates some relatively difficult decisions with respect to the sampling of the aliphatic fingerprint spectrum. In this sample there is a convenient place for folding the spectrum, but still the indirect 13Cα dimension is only sampled to about half the digital resolution of the other two spectra. This causes the resolution to be worse in the more crowded spectrum, which is not an ideal situation. It should be possible to extend the chemical shift evolution or even implement non-uniform sampling by calculating the timings and phases necessary. The sampling of the 13Cα chemical shift dimension could also be extended so that the experiment is collected in any number of blocks containing different increments for the indirect dimension, and then each portion concatenated onto the last, where the relaxation time is repeated the appropriate number of times for packing of the experiments. The method used here to split and rearrange the experiments should be valid under different experimental conditions. For example, in triply labelled [2H, 13C, 15N] and back-exchanged samples at slower spinning, the amide proton may be used exclusively as the read-out nucleus since the CP is efficient and fairly predictable amongst the three backbone nuclei: the amide, alpha carbon and carbonyl carbon. In this case, the COSY transfer in the 13C′ experiment would be removed in favor of a simple CP back to the amide proton. For site specific R1 measurements the aliphatic carbons could be made accessible at 50/60 kHz MAS through a combination of alternate 13C labelling and extensive deuteration,35 and at > 80 kHz with alternate 13C labelling.34
Footnotes |
† Electronic supplementary information (ESI) available. See DOI: https://doi.org/10.1039/d2cp03458a |
‡ These authors contributed equally to this work. |
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