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Materials Data on Tb5Rh3 by Materials Project

Tb5Rh3 crystallizes in the hexagonal P6_3/mcm space group. The structure is three-dimensional. there are two inequivalent Tb sites. In the first Tb site, Tb is bonded to six equivalent Rh atoms to form a mixture of distorted corner, edge, and face-sharing TbRh6 octahedra. The corner-sharing octahedral tilt angles are 35°. All Tb–Rh bond lengths are 3.02 Å. In the second Tb site, Tb is bonded in a 5-coordinate geometry to five equivalent Rh atoms. There are a spread of Tb–Rh bond distances ranging from 2.88–3.37 Å. Rh is bonded in a 9-coordinate geometry to nine Tb atoms.

36 MATERIALS SCIENCE↗

Materials Data on Tb5Bi3 by Materials Project

Tb5Bi3 crystallizes in the hexagonal P6_3/mcm space group. The structure is three-dimensional. there are two inequivalent Tb sites. In the first Tb site, Tb is bonded in a 6-coordinate geometry to six equivalent Bi atoms. All Tb–Bi bond lengths are 3.28 Å. In the second Tb site, Tb is bonded in a 5-coordinate geometry to five equivalent Bi atoms. There are a spread of Tb–Bi bond distances ranging from 3.14–3.45 Å. Bi is bonded in a 9-coordinate geometry to nine Tb atoms.

36 MATERIALS SCIENCE↗

Materials Data on TbMnAl by Materials Project

TbMnAl is Hexagonal Laves-derived structured and crystallizes in the orthorhombic Imma space group. The structure is three-dimensional. Tb is bonded in a 12-coordinate geometry to four equivalent Tb, six equivalent Mn, and six equivalent Al atoms. There are two shorter (3.32 Å) and two longer (3.40 Å) Tb–Tb bond lengths. There are two shorter (3.12 Å) and four longer (3.27 Å) Tb–Mn bond lengths. There are four shorter (3.21 Å) and two longer (3.22 Å) Tb–Al bond lengths. Mn is bonded to six equivalent Tb, two equivalent Mn, and four equivalent Al atoms to form MnTb6Mn2Al4 cuboctahedra that share corners with eight equivalent AlTb6Mn4Al2 cuboctahedra, corners with ten equivalent MnTb6Mn2Al4 cuboctahedra, edges with six equivalent MnTb6Mn2Al4 cuboctahedra, faces with six equivalent MnTb6Mn2Al4 cuboctahedra, and faces with twelve equivalent AlTb6Mn4Al2 cuboctahedra. Both Mn–Mn bond lengths are 2.75 Å. All Mn–Al bond lengths are 2.73 Å. Al is bonded to six equivalent Tb, four equivalent Mn, and two equivalent Al atoms to form AlTb6Mn4Al2 cuboctahedra that share corners with eight equivalent MnTb6Mn2Al4 cuboctahedra, corners with ten equivalent AlTb6Mn4Al2 cuboctahedra, edges with six equivalent AlTb6Mn4Al2 cuboctahedra, faces with six equivalent AlTb6Mn4Al2 cuboctahedra, and faces with twelve equivalent MnTb6Mn2Al4 cuboctahedra. Both Al–Al bond lengths are 2.79 Å.

36 MATERIALS SCIENCE↗

Materials Data on Tb5Sn3 by Materials Project

Tb5Sn3 crystallizes in the hexagonal P6_3/mcm space group. The structure is three-dimensional. there are two inequivalent Tb sites. In the first Tb site, Tb is bonded in a 6-coordinate geometry to six equivalent Sn atoms. All Tb–Sn bond lengths are 3.23 Å. In the second Tb site, Tb is bonded in a 5-coordinate geometry to five equivalent Sn atoms. There are a spread of Tb–Sn bond distances ranging from 3.10–3.58 Å. Sn is bonded in a 9-coordinate geometry to nine Tb atoms.

36 MATERIALS SCIENCE↗

Materials Data on Tb2Mn3Al by Materials Project

Tb2Mn3Al is Hexagonal Laves-derived structured and crystallizes in the trigonal R-3m space group. The structure is three-dimensional. Tb is bonded in a 12-coordinate geometry to four equivalent Tb, nine equivalent Mn, and three equivalent Al atoms. There are one shorter (3.20 Å) and three longer (3.34 Å) Tb–Tb bond lengths. There are three shorter (3.13 Å) and six longer (3.16 Å) Tb–Mn bond lengths. All Tb–Al bond lengths are 3.19 Å. Mn is bonded to six equivalent Tb, four equivalent Mn, and two equivalent Al atoms to form MnTb6Mn4Al2 cuboctahedra that share corners with four equivalent AlTb6Mn6 cuboctahedra, corners with fourteen equivalent MnTb6Mn4Al2 cuboctahedra, edges with six equivalent MnTb6Mn4Al2 cuboctahedra, faces with six equivalent AlTb6Mn6 cuboctahedra, and faces with twelve equivalent MnTb6Mn4Al2 cuboctahedra. All Mn–Mn bond lengths are 2.72 Å. Both Mn–Al bond lengths are 2.67 Å. Al is bonded to six equivalent Tb and six equivalent Mn atoms to form AlTb6Mn6 cuboctahedra that share corners with six equivalent AlTb6Mn6 cuboctahedra, corners with twelve equivalent MnTb6Mn4Al2 cuboctahedra, edges with six equivalent AlTb6Mn6 cuboctahedra, and faces with eighteen equivalent MnTb6Mn4Al2 cuboctahedra.

36 MATERIALS SCIENCE↗

Materials Data on Tb3Mn3Ga2Ge by Materials Project

Tb3Mn3GeGa2 crystallizes in the hexagonal P-6 space group. The structure is three-dimensional. Tb is bonded in a 5-coordinate geometry to six equivalent Mn, three Ga, and two equivalent Ge atoms. There are a spread of Tb–Mn bond distances ranging from 3.22–3.32 Å. There are one shorter (2.94 Å) and two longer (2.98 Å) Tb–Ga bond lengths. Both Tb–Ge bond lengths are 2.96 Å. Mn is bonded in a 12-coordinate geometry to six equivalent Tb, two equivalent Mn, three Ga, and one Ge atom. Both Mn–Mn bond lengths are 2.86 Å. There are two shorter (2.66 Å) and one longer (2.78 Å) Mn–Ga bond lengths. The Mn–Ge bond length is 2.75 Å. There are two inequivalent Ga sites. In the first Ga site, Ga is bonded in a 9-coordinate geometry to six equivalent Tb and three equivalent Mn atoms. In the second Ga site, Ga is bonded in a distorted q6 geometry to three equivalent Tb and six equivalent Mn atoms. Ge is bonded in a 9-coordinate geometry to six equivalent Tb and three equivalent Mn atoms.

36 MATERIALS SCIENCE↗

Materials Data on TbB2Rh3 by Materials Project

TbRh3B2 crystallizes in the hexagonal P6/mmm space group. The structure is three-dimensional. Tb is bonded in a 12-coordinate geometry to two equivalent Tb, twelve equivalent Rh, and six equivalent B atoms. Both Tb–Tb bond lengths are 3.14 Å. All Tb–Rh bond lengths are 3.14 Å. All Tb–B bond lengths are 3.14 Å. Rh is bonded in a distorted square co-planar geometry to four equivalent Tb and four equivalent B atoms. All Rh–B bond lengths are 2.22 Å. B is bonded in a 6-coordinate geometry to three equivalent Tb and six equivalent Rh atoms.

36 MATERIALS SCIENCE↗

Materials Data on Tb4BClO7 by Materials Project

Tb4BO7Cl crystallizes in the monoclinic P2_1/c space group. The structure is three-dimensional. there are four inequivalent Tb3+ sites. In the first Tb3+ site, Tb3+ is bonded in a 6-coordinate geometry to six O2- and one Cl1- atom. There are a spread of Tb–O bond distances ranging from 2.23–2.36 Å. The Tb–Cl bond length is 3.16 Å. In the second Tb3+ site, Tb3+ is bonded in a 7-coordinate geometry to six O2- and one Cl1- atom. There are a spread of Tb–O bond distances ranging from 2.29–2.44 Å. The Tb–Cl bond length is 3.01 Å. In the third Tb3+ site, Tb3+ is bonded in a 8-coordinate geometry to seven O2- and one Cl1- atom. There are a spread of Tb–O bond distances ranging from 2.26–2.81 Å. The Tb–Cl bond length is 3.20 Å. In the fourth Tb3+ site, Tb3+ is bonded in a 5-coordinate geometry to five O2- and two equivalent Cl1- atoms. There are a spread of Tb–O bond distances ranging from 2.22–2.37 Å. There are one shorter (2.96 Å) and one longer (3.20 Å) Tb–Cl bond lengths. B3+ is bonded in a trigonal planar geometry to three O2- atoms. There are a spread of B–O bond distances ranging from 1.37–1.39 Å. There are seven inequivalent O2- sites. In the first O2- site, O2- is bonded to four Tb3+ atoms to form a mixture of edge and corner-sharing OTb4 tetrahedra. In the second O2- site, O2- is bonded to four Tb3+ atoms to form a mixture of edge and corner-sharing OTb4 tetrahedra. In the third O2- site, O2- is bonded in a 1-coordinate geometry to three Tb3+ and one B3+ atom. In the fourth O2- site, O2- is bonded in a distorted trigonal planar geometry to two Tb3+ and one B3+ atom. In the fifth O2- site, O2- is bonded in a distorted single-bond geometry to three Tb3+ and one B3+ atom. In the sixth O2- site, O2- is bonded to four Tb3+ atoms to form a mixture of edge and corner-sharing OTb4 tetrahedra. In the seventh O2- site, O2- is bonded to four Tb3+ atoms to form a mixture of distorted edge and corner-sharing OTb4 tetrahedra. Cl1- is bonded in a 2-coordinate geometry to five Tb3+ atoms.

36 MATERIALS SCIENCE↗

Materials Data on TbTiFe11C by Materials Project

TbTiFe11C crystallizes in the orthorhombic Imm2 space group. The structure is three-dimensional. Tb is bonded in a distorted linear geometry to one Ti, ten Fe, and two equivalent C atoms. The Tb–Ti bond length is 3.17 Å. There are a spread of Tb–Fe bond distances ranging from 3.07–3.30 Å. Both Tb–C bond lengths are 2.44 Å. Ti is bonded in a 1-coordinate geometry to one Tb and thirteen Fe atoms. There are a spread of Ti–Fe bond distances ranging from 2.36–2.95 Å. There are six inequivalent Fe sites. In the first Fe site, Fe is bonded in a single-bond geometry to six Fe and one C atom. There are four shorter (2.46 Å) and two longer (2.64 Å) Fe–Fe bond lengths. The Fe–C bond length is 1.89 Å. In the second Fe site, Fe is bonded in a single-bond geometry to two equivalent Ti, six Fe, and one C atom. There are four shorter (2.48 Å) and two longer (2.65 Å) Fe–Fe bond lengths. The Fe–C bond length is 1.91 Å. In the third Fe site, Fe is bonded in a single-bond geometry to one Ti, six Fe, and one C atom. There are a spread of Fe–Fe bond distances ranging from 2.44–2.71 Å. The Fe–C bond length is 1.89 Å. In the fourth Fe site, Fe is bonded to two equivalent Tb, one Ti, and nine Fe atoms to form distorted FeTb2TiFe9 cuboctahedra that share corners with ten equivalent FeTb2TiFe9 cuboctahedra, corners with two equivalent CTb2Fe4 octahedra, edges with four equivalent FeTb2TiFe9 cuboctahedra, faces with six equivalent FeTb2TiFe9 cuboctahedra, and faces with two equivalent CTb2Fe4 octahedra. The corner-sharing octahedra tilt angles range from 67–69°. There are a spread of Fe–Fe bond distances ranging from 2.43–2.63 Å. In the fifth Fe site, Fe is bonded in a 1-coordinate geometry to one Ti and eight Fe atoms. All Fe–Fe bond lengths are 2.98 Å. In the sixth Fe site, Fe is bonded in a 12-coordinate geometry to one Tb, two equivalent Ti, and eleven Fe atoms. The Fe–Fe bond length is 2.41 Å. C is bonded to two equivalent Tb and four Fe atoms to form CTb2Fe4 octahedra that share corners with eight equivalent FeTb2TiFe9 cuboctahedra, corners with two equivalent CTb2Fe4 octahedra, and faces with eight equivalent FeTb2TiFe9 cuboctahedra. The corner-sharing octahedral tilt angles are 2°.

36 MATERIALS SCIENCE↗

Mesoscale Convective Systems Represented in High Resolution E3SMv2 and Impact of New Cloud and Convection Parameterizations

Mesoscale convective systems (MCSs) play an important role in modulating the global hydrological cycle, general circulation, and radiative energy budget. In this study, we evaluate MCS simulations in the second version of U.S. Department of Energy (DOE) Energy Exascale Earth System Model (E3SMv2). E3SMv2 atmosphere model (EAMv2) is run at the uniform 0.25? horizontal resolution. We track MCSs consistently in the model and observations using the PyFLEXTRKR algorithm, which defines MCS based on both cloud-top brightness temperature (Tb) and surface precipitation. Results from using Tb only to define MCS, commonly used in previous studies, are also discussed. Furthermore, sensitivity experiments are performed to examine the impact of new cloud and convection parameterizations developed for EAMv3 on simulated MCSs. Our results show that EAMv2 simulated MCS precipitation is largely underestimated in the tropics and contiguous United States. This is mainly attributed to the underestimated precipitation intensity in EAMv2. In contrast, the simulated MCS frequency becomes more comparable to observations if MCSs are defined only based on cloud-top Tb. The Tb-based MCS tracking method, however, includes many cloud systems with very weak precipitation which conflicts with the MCS definition. This result illustrates the importance of accounting for precipitation in evaluating simulated MCSs. We also find that the new physics parameterizations help increase the relative contribution of convective precipitation to total precipitation in the tropics, but the simulated MCS properties are generally not improved. This suggests that simulating MCSs will remain a challenge for the next version of E3SM.

Zhang, Meng↗

Quantitative insights into the dislocation source behavior of twin boundaries suggest a new dislocation source mechanism

Pop-in statistics from nanoindentation with spherical indenters are used to determine the stress required to activate dislocation sources in twin boundaries (TBs) in copper and its alloys. The TB source activation stress is smaller than that needed for bulk single crystals, irrespective of the indenter size, dislocation density and stacking fault energy. Because an array of pre-existing Frank partial dislocations is present at a TB, we propose that dislocation emission from the TB occurs by the Frank partials splitting into Shockley partials moving along the TB plane and perfect lattice dislocations, both of which are mobile. The proposed mechanism is supported by recent high resolution transmission electron microscopy images in deformed nanotwinned (NT) metals and may help to explain some of the superior properties of nanotwinned metals (e.g. high strength and good ductility), as well as the process of detwinning by the collective formation and motion of Shockley partial dislocations along TBs.

36 MATERIALS SCIENCE↗

Endogenous thermoregulatory rhythms of squirrel monkeys in thermoneutrality and cold

Whole body heat production (HP) and heat loss (HL) were examined to determine if the free-running circadian rhythm in body temperature (Tb) results from coordinated changes in HP and HL rhythms in thermoneutrality (27 degrees C) as well as mild cold (17 degrees C). Squirrel monkey metabolism (n = 6) was monitored by both indirect and direct calorimetry, with telemetered measurement of Tb and activity. Feeding was also measured. Rhythms of HP, HL, and conductance were tightly coupled with the circadian Tb rhythm at both ambient temperatures (TA). At 17 degrees C, increased HP compensated for higher HL at all phases of the Tb rhythm, resulting in only minor changes to Tb. Parallel compensatory changes of HP and HL were seen at all rhythm phases at both TA. Similar time courses of Tb, HP, and HL in their respective rhythms and the relative stability of Tb during both active and rest periods suggest action of the circadian timing system on Tb set point.

NASA Discipline Regulatory Physiology↗

Estimating Rain Rates from Tipping-Bucket Rain Gauge Measurements

This paper describes the cubic spline based operational system for the generation of the TRMM one-minute rain rate product 2A-56 from Tipping Bucket (TB) gauge measurements. Methodological issues associated with applying the cubic spline to the TB gauge rain rate estimation are closely examined. A simulated TB gauge from a Joss-Waldvogel (JW) disdrometer is employed to evaluate effects of time scales and rain event definitions on errors of the rain rate estimation. The comparison between rain rates measured from the JW disdrometer and those estimated from the simulated TB gauge shows good overall agreement; however, the TB gauge suffers sampling problems, resulting in errors in the rain rate estimation. These errors are very sensitive to the time scale of rain rates. One-minute rain rates suffer substantial errors, especially at low rain rates. When one minute rain rates are averaged to 4-7 minute or longer time scales, the errors dramatically reduce. The rain event duration is very sensitive to the event definition but the event rain total is rather insensitive, provided that the events with less than 1 millimeter rain totals are excluded. Estimated lower rain rates are sensitive to the event definition whereas the higher rates are not. The median relative absolute errors are about 22% and 32% for 1-minute TB rain rates higher and lower than 3 mm per hour, respectively. These errors decrease to 5% and 14% when TB rain rates are used at 7-minute scale. The radar reflectivity-rainrate (Ze-R) distributions drawn from large amount of 7-minute TB rain rates and radar reflectivity data are mostly insensitive to the event definition.

Wang, Jianxin↗

The Radiative Consistency of Atmospheric Infrared Sounder and Moderate Resolution Imaging Spectroradiometer Cloud Retrievals

The consistency of cloud top temperature (Tc) and effective cloud fraction (f) retrieved by the Atmospheric Infrared Sounder (AIRS)/Advanced Microwave Sounding Unit (AMSU) observation suite and the Moderate Resolution Imaging Spectroradiometer (MODIS) on the EOS-Aqua platform are investigated. Collocated AIRS and MODIS TC and f are compared via an 'effective scene brightness temperature' (Tb,e). Tb,e is calculated with partial field of view (FOV) contributions from TC and surface temperature (TS), weighted by f and 1-f, respectively. AIRS reports up to two cloud layers while MODIS reports up to one. However, MODIS reports TC, TS, and f at a higher spatial resolution than AIRS. As a result, pixel-scale comparisons of TC and f are difficult to interpret, demonstrating the need for alternatives such as Tb,e. AIRS-MODIS Tb,e differences ((Delta)Tb,e) for identical observing scenes are useful as a diagnostic for cloud quantity comparisons. The smallest values of DTb,e are for high and opaque clouds, with increasing scatter in (Delta)Tb,e for clouds of smaller opacity and lower altitude. A persistent positive bias in DTb,e is observed in warmer and low-latitude scenes, characterized by a mixture of MODIS CO2 slicing and 11-mm window retrievals. These scenes contain heterogeneous cloud cover, including mixtures of multilayered cloudiness and misplaced MODIS cloud top pressure. The spatial patterns of (Delta)Tb,e are systematic and do not correlate well with collocated AIRS-MODIS radiance differences, which are more random in nature and smaller in magnitude than (Delta)Tb,e. This suggests that the observed inconsistencies in AIRS and MODIS cloud fields are dominated by retrieval algorithm differences, instead of differences in the observed radiances. The results presented here have implications for the validation of cloudy satellite retrieval algorithms, and use of cloud products in quantitative analyses.

clouds↗

Olivine Dissolution and Formation of Secondary phases in Ultramafic Soils

Introduction: Olivine has been proposed as an indicator for the duration of water-rock interaction within Martian rocks and sediments [1-3]. The use of olivine as a mineralogical indicator for past aqueous alteration on Mars requires interpretation of a complex combination of factors including pH, temperature, and composition [5,6]. Here, we examine the persistence of natural olivine within terrestrial ultramafic soils (Fe/Mg-rich, Al-poor) developing under different climatic conditions and the incipient dissolution of emplaced forsterite (Fo) and fayalite (Fa) surfaces to investigate environmental effects on incipient olivine dissolution, olivine persistence in soils, and formation of secondary phases. Methods: Field Sites. We examined olivine weathering and secondary material formation in ultramafic soils at 6 sites in the Klamath Mountains (KM) of northern California with a mean annual temperature of ~12.8℃ and precipitation of ~55.7-95.4 cm/year [7], and soil pH of ~6.5-7.3; 4 sites in the Tablelands (TB) of Newfoundland, Canada with a mean annual temperature of <3.9℃ and precipitation of ~120.0 cm/year [8], and soil pH of ~7.7; and at 3 sites at Pickhandle Gulch (PG), Nevada with a mean annual temperature of ~14.4℃ and precipitation of ~14.1 cm/year [7], and soil pH of ~8.5. Sampling sites span an age range of ~12.1-50+ kya in the Klamath Mountains [9,10] and ~13-30 kya in the Tablelands [11]. Pickhandle Gulch sites are undated. Parent Material and Soil Analyses. Polished thin sections of bulk soil prepared by Wagner Petrographic, Inc were carbon-coated and analyzed on a JEOL 2100 SEM in back-scattered electron mode in the EMIL lab at UNLV and at the 13-ID-E synchrotron beamline at Argonne National Laboratory using µXRF, µXRD, and XAS. Soil and parent material samples were powdered in a Fritsch pulverisette and analyzed by XRD and soil by VNIR. Soil preparation is further described in [12]. Disk Preparation, Burial, and Collection. Fo disks were cut from a column prepared via hot-pressing and Fa disks by sintering synthetic fayalite powder, see [13] for detail. Disks were polished to a 0.25-micron level with diamond grit. Disks were buried in 3 KM soils, 4 TB soils, and 3 PG soils, collected after exactly 365 days, and washed gently with 100% reagent grade ethanol to remove potential adhered soil material. Weathered disks and soil samples were stored in a -20℃ freezer until analysis. Unaltered control disks prepared identically to the buried disks were stored at -20℃ for the duration of the experiment. Disk Analyses. One Fo and Fa disk from each climate zone was analyzed on a variable pressure Zeiss Supra 40VP SEM at Northern Arizona University. A separate Fo and Fa disk from each climate zone was analyzed by XPS using a Physical Electronics VersaProbe II at the Penn State Univ. Materials Characterization Lab after a Na-dodecyl sulfate wash and ozonation to remove carbon contamination as in [14]. VNIR measurements were conducted at Johnson Space Center using an ASD FieldSpec3 under ambient lab conditions on a separate Fo and Fa disk from each climate zone. One separate Fo and Fa control sample was analyzed for each technique for comparison with weathered samples. XPS uncertainty was determined from 5 repeat measurements on controls. Results: Bedrock and Soil Results Olivine is present in the parent material in the KM and TB. Olivine is found in ~12.1 ka KM soils but is absent from all older soils, while persisting into the oldest (>20 ka) TB soil (Figure 1). In both locations, olivine is found as cores surrounded by a serpentine rind (Figure 2). VNIR spectra from the analyzed soils possess strong OH-associated spectral features at ~2.33 µm indicating the presence of Mg-rich phyllosilicates as well as ferric-oxide features at ~0.92 µm in the KM (Figure 3). Primary crystalline silicate grains mostly incorporate Fe2+, while poorly crystalline weathering rinds are best fit by ferric oxide XAS standards (Figure 4). µXRF also shows that Fe and Ni concentrate in weathering rinds and Cr remains within interior silicate grains (Figure 4). Buried Sample Results All Fo surfaces exhibited formation of dissolution features including shallow pitting not observed on controls. Dissolution features were most visually widespread on the KM disk (Figure 5). Leaching of Mg from KM and TB Fo disks was evident from <1.6 Mg/Si ratios measured by XPS (Figure 6). Fe-rich precipitates in SEM (Figure 5) and Fe presence in XPS scans (Figure 6) indicate Fe deposition onto KM and TB Fo disk surfaces. The appearance of a spectral feature at 0.55 µm in the VNIR spectra from the TB Fo suggests this Fe is ferric (Figure 7). The PG Fo appears least altered, with minimal formation of dissolution features in SEM (Figure 5), a Mg/Si ratio inconsistent with leaching (~2) (Figure 6), and VNIR spectra almost identical to the control sample. Analysis of Fa surfaces is ongoing. The higher temperatures and more acidic pH in the KM soils likely drive the faster dissolution of the Fo disks described above. While the TB soils experience greater precipitation than in the KM, the cooler temperatures and more basic soil pH facilitate observable but more limited alteration. The dry climate and basic soil pH at PG lead to minimal dissolution of the PG disk surfaces.

A D Feldman↗

Evaluating The Relationships Between Supine Propriorception Assessments with Upright Functional Mobility and Balance Tests

INTRODUCTION Upon return to Earth, spaceflight sensorimotor adaptations can result in impaired posture and locomotion [1], [2], and current exercise countermeasures in the International Space Station are not sufficient to maintain sensorimotor function. In-flight countermeasures and assessment tools for sensorimotor function are needed to mitigate risks associated with mission-critical task performance upon return to Earth or arrival to 0.38 G on Mars. One proposed countermeasure for proprioceptive deconditioning includes training on a tilt board device [3], which will be tested in an upcoming bed rest study. In preparation for the said study, the objective of this pilot study is to compare performance in supine proprioceptive assessments to performance in functional upright activities. The results are intended to guide the selection of supine assessment tools for the upcoming bedrest study and the development of future inflight proprioceptive training and assessment tools for exploration missions. METHODS Seventeen healthy participants (8 males and 9 females, 27.9 ± 8.5 years) provided informed consent as approved by the Institutional Review Board (IRB) at NASA. A horizontal air-bearing sled was used to provide a proprioceptive challenge in a supine body orientation, allowing for mediolateral motion with minimal friction during supine stance [4]. Participants were loaded axially (30 to 60% body weight) with their feet on a vertically oriented tilt board and instructed to perform supine assessment activities using custom software that displays a cursor controlled by tilting the tilt board. In a single-leg static activity on the tilt board (TB-St), performance was measured as the percent time spent on a center target during a 30-second trial. During a two-feet dynamic activity on the tilt board (TB-Dy), performance was measured as the number of targets captured in 30 seconds. These supine tasks were compared to performance during two upright activities used to represent upright performance: completion time for a functional mobility task (FMT) [2],[5] and a performance score from force plate sway data during 30-second single-leg upright standing (USL). RESULTS AND DISCUSSION A Spearman's rank-order correlation was run to assess the relationship between upright and supine assessments. There were statistically significant, strong correlations between scores for the FMT and each TB activity, including TB-St, rs(17) = 0.50, p<0.05, TB-Dy3, rs(17) = 0.73, p<0.001, and TB-Dy9, rs(15) = 0.53, p<0.05. There were no statistically significant correlations between USL and each TB activity. Despite a lack of correlation with upright single-leg balance, the ability of the TB to indicate upright performance in the FMT is promising, as this task is a standard post-flight measure designed to characterize locomotor dysfunction [2], [5]. CONCLUSION These efforts will inform the selection of an appropriate sensorimotor assessment method for the upcoming bed rest study and similar future studies. While current work uses a bed rest analog to develop these technologies, future work aims to prepare capabilities for future in-flight sensorimotor training and assessment to mitigate the risks of proprioception impairment after spaceflight. ACKNOWLEDGEMENTS This work was supported by the University Space Research Association Internship Program. REFERENCES [1] Mulavara A.P. et al (2018) Med Sci Sports Exerc, 50(9), 1961-1980. [2] Mulavara A.P. et al (2010) Exp Brain Res, 202(3), 649-659. [3] Macaulay T.R. et al (2021) Front. Syst. Neurosci., 15, 658-985. [4] Goel R. et al (2017) Front. Syst. Neurosci, 11. [5] Koppelmans V. et al (2013) BMC Neurology, 12.

R Bellisle↗

Materials Data on Tb4CoB13 by Materials Project

Tb4CoB13 crystallizes in the tetragonal P4/mnc space group. The structure is three-dimensional. Tb+3.25+ is bonded in a 6-coordinate geometry to one Co2+ and fifteen B+1.15- atoms. The Tb–Co bond length is 2.70 Å. There are a spread of Tb–B bond distances ranging from 2.59–2.92 Å. Co2+ is bonded in a 12-coordinate geometry to four equivalent Tb+3.25+ and eight equivalent B+1.15- atoms. All Co–B bond lengths are 2.18 Å. There are three inequivalent B+1.15- sites. In the first B+1.15- site, B+1.15- is bonded in a 9-coordinate geometry to four equivalent Tb+3.25+, one Co2+, and four B+1.15- atoms. There is three shorter (1.80 Å) and one longer (2.13 Å) B–B bond length. In the second B+1.15- site, B+1.15- is bonded in a cuboctahedral geometry to four equivalent Tb+3.25+ and eight equivalent B+1.15- atoms. In the third B+1.15- site, B+1.15- is bonded in a 3-coordinate geometry to six equivalent Tb+3.25+ and three B+1.15- atoms. The B–B bond length is 1.89 Å.

36 MATERIALS SCIENCE↗

Materials Data on Tb3Mn3Ga2Si by Materials Project

Tb3Mn3Ga2Si crystallizes in the hexagonal P-62m space group. The structure is three-dimensional. Tb is bonded in a 5-coordinate geometry to six equivalent Mn, four equivalent Ga, and one Si atom. There are four shorter (3.19 Å) and two longer (3.34 Å) Tb–Mn bond lengths. All Tb–Ga bond lengths are 2.93 Å. The Tb–Si bond length is 2.89 Å. Mn is bonded in a 12-coordinate geometry to six equivalent Tb, two equivalent Mn, two equivalent Ga, and two equivalent Si atoms. Both Mn–Mn bond lengths are 2.72 Å. Both Mn–Ga bond lengths are 2.88 Å. Both Mn–Si bond lengths are 2.52 Å. Ga is bonded in a 9-coordinate geometry to six equivalent Tb and three equivalent Mn atoms. Si is bonded in a 9-coordinate geometry to three equivalent Tb and six equivalent Mn atoms.

36 MATERIALS SCIENCE↗