Sr Data Research Articles

Extending WiMDA for the data analysis of µ −SR experiments

A software extension to the Windows Muon Data Analysis software package WiMDA has been developed for the analysis of µ −SR data, which has been dubbed Negative-WiMDA. In designing Negative-WiMDA, some key features were considered: it should be easily accessed from the main analysis window of WiMDA; it should be able to account for multiple elements in a sample; it should be able to subtract signals treated as unwanted background, allowing the user to focus on a particular element of interest; it should be able to handle transverse-field (TF) data, and perhaps most importantly, it should be intuitive to use. The main features of Negative-WiMDA are presented here with a few examples of their use.

Evolution of short-range magnetic correlations in ferromagnetic Ni-V alloys

We experimentally study how the magnetic correlations develop in a binary alloy close to the ferromagnetic quantum critical point with small-angle neutron scattering (SANS). Upon alloying the itinerant ferromagnet nickel with vanadium, the ferromagnetic order is continuously suppressed. The critical temperature Tc vanishes when vanadium concentrations reach the critical value of xc=0.116 indicating a quantum critical point separating the ferromagnetic and paramagnetic phases. Earlier magnetization and $\mu$SR data have indicated the presence of magnetic inhomogeneities in Ni(1-x)V(x) and, in particular, recognize the magnetic clusters close to xc, on the paramagnetic and on the ferromagnetic sides with nontrivial dynamical properties [R. Wang et al., Phys. Rev. Lett. 118, 267202 (2017)]. We present the results of SANS study with full polarization analysis of polycrystalline Ni(1-x)V(x) samples with x=0.10 and x=0.11 with low critical temperatures Tc below 50 K. For both Ni-V samples close to xc we find isotropic magnetic short-range correlations in the nanometer-scale persisting at low temperatures. They are suppressed gradually in higher magnetic fields. In addition, signatures of long-range ordered magnetic domains are present below Tc. The fraction of these magnetic clusters embedded in the ferromagnetic ordered phase grows towards xc and agrees well with the cluster fraction estimate from the magnetization and $\mu$SR data. Our SANS studies provide new insights into the nature of the inhomogeneities in a ferromagnetic alloy close to a quantum critical point.

Study of polarization data for Sr(1-2x)NaxNdxBi4Ti4O15 ceramics prepared through sol-gel route: An experimental and simulation using modified Glazounov equation

Sr(1-2x)NaxNdxBi4Ti4O15 (x = 0.0, 0.1, 0.2, 0.4 & 0.5) ceramic samples were fabricatedusing sol–gel route. The variations of polarization as a function of electric filed (PE loops) were calculated at various concentration and temperatures. Simulation of polarization data using modified Glazounov equation as proposed by us earlier was carried out. The activation energy induced by electric field and thermally activated orientation of dipoles were calculated using modified Glazounov equation. This equation also gives information about the dipole moment. The value of dipole moment for ceramic samples with x = 0.0 is 3.53x10-26C.m and this value increases with the increase of × value and the dipole moment value at × = 0.5was 6.36x10-26C.m. The increase of dipole moment with the change of concentration and temperature was due to smaller average ionic radii of Na (116 pm) and Nd (143 pm) when compared to ionic radii of Sr (132 pm) causing larger displacement of ions at A site with the doping of Na and Nd at Sr site.

90Sr and stable element levels in bones of brown bears: long-term trends in bear populations from Croatia and Poland.

The aim of this study was to investigate the temporal trends and geographical differences in 90Sr and stable element (Ba, Ca, Mn, Sr, Pb, Zn) levels in the bones of Croatian and Polish brown bear (Ursus arctos) populations. Experimental data suggest that in the decades after nuclear weapon tests and the Chernobyl accident, 90Sr bone activity concentrations decreased from 352 to 11Bqkg-1 in the Croatian bear population (period 1982-2015) and from 831 to 27Bqkg-1 in Polish bears (period 1962-2020). Calculated effective and ecological half-lives were 9 and 13years for Croatian bears, and 15 and 31years for Polish bears, respectively. Different temporal trends were noted in levels of Ba, Mn, Pb and Zn between the two countries with majority of bones having lower Pb, Sr and Zn in Croatian than in Polish bears. Estimated values for the soil-to-bear transfer of 90Sr were the same order of magnitude in the studied populations. Contrary to this, the estimated transfer of stable Sr was an order of magnitude lower for the Croatian bear population compared to Polish bears. The observed differences in soil-to-bear transfer between stable Sr and 90Sr found for Croatian bears might suggest the need for careful consideration on the use of stable Sr data as an analogue for 90Sr. To our knowledge, this is the first study that analysed 90Sr activity in tissue of brown bears. As such, it provides insight into the fate and behaviour of one of the most relevant anthropogenic radionuclides at the top of the food chain.

A data plane security model of SR-BE/TE based on zero-trust architecture

Facing the untrusted threats of network elements and PKI/CA faced by SR-BE/TE (Segment Routing-BE/TE) data plane in the zero-trust network environment, firstly, this paper refines it into eight specific security issues. Secondly, an SR-BE/TE data plane security model ZbSR (ZTA-based SR) based on zero-trust architecture is proposed, which reconstructs the original SR control plane into a "trust-agent" two-layer plane based on 4 components of the controller, agent, cryptographic center and information base. On one hand, we distinguish between the two segment list generation modes and proposes corresponding data exchange security algorithms, by introducing north–south security verification based on identity authentication, trust evaluation, and key agreement before the terminal device establishes an east–west access connection, so reliable data exchange between terminal devices can be realized. On the other hand, for the network audit lacking SR-BE/TE, a network audit security algorithm based on solid authentication is proposed. By auditing the fields, behaviors, loops, labels, paths, and SIDs of messages, threats such as stream path tampering, SID tampering, DoS attacks, and loop attacks can be effectively detected. Finally, through the simulation test, the proposed model can provide security protection for the SR data plane with a 19.3% average incremental delay overhead for various threat scenarios.

Genome-Wide Methylation and Haplotype-Resolved Aberrant Somatic Hypermutation Patterns in B-Cell Lymphomas

Introduction Diffuse large B-cell lymphoma (DLBCL) is a genetically, phenotypically, and clinically heterogenous disease. Multiple molecular classification systems using either genomic aberrations or gene expression profiles are used to delineate subgroups with shared biology. The cell of origin (COO) gene expression-based classification system stratifies DLBCLs into germinal center B-cell-like (GCB) and activated B-cell-like subgroups of DLBCL. More recently, the double-hit signature (DHITsig) has been used to further stratify GCB DLBCLs into DHITsig+ and DHITsig-, where the former is characterized by a gene expression profile reminiscent of the GC dark zone and inferior outcomes. Currently, patterns of somatic driver mutations can only partially explain the expression of DHITsig in some tumors. Genetic features such as DNA methylation have been shown to be associated with transcriptional repression and altered chromatin structure. We hypothesized that resolving DNA methylation patterns genome-wide using long read whole genome sequencing (LR-WGS) may reveal epigenetic differences associated with differential gene expression profiles within the DHITsig+ and DHITsig- subgroups and in the context of histologic transformation from follicular lymphoma. Methods Whole genome sequencing data of 10 patient samples and 4 cell line GCB DLBCL samples were generated using both short read (SR-WGS; Illumina) and LR-WGS (Oxford Nanopore Technologies, PromethION). The complementary approach combines somatic variant calling from highly accurate SR data with DNA methylation calling from LR data. GCB samples were selected based on the NanoString DLBCL90 assay and further subdivided into DHITsig+ (N=4) and DHITsig- (N=3). RNA sequencing data of 9 patient samples and 3 GCB DLBCL cell lines were generated and analyzed using Salmon and DESeq2. Simple somatic mutations from SR-WGS data were called using an ensemble of somatic variant callers, which confirmed all cases to belong to the EZB genetic subgroup. Methylated bases were called with Nanopolish followed by a differential methylation analysis using the DSS package in R to identify differences in methylation between both subgroups. Differentially methylated regions (DMRs) were annotated for GC B-cell specific superenhancers, CpG islands, and genes. Using WhatsHap and Nanomethphase, heterozygous single nucleotide polymorphisms (SNPs) from SR and LR data were used to phase LRs into haplotypes. Haplotype analyses were performed to determine the phase of aberrant somatic hypermutation (aSHM) and methylation patterns in the context of proximal translocation breakpoints. Results Most DMRs were found to be associated with regulatory regions such as promoters, superenhancers, and CpG islands. We found methylation differences between DHITsig+ and DHITsig- subgroups in 1430 superenhancers known to be active in GC B-cells. Within these superenhancer regions, DHITsig+ tumors were typically hypomethylated relative to DHITsig-. Several DHITsig classifier genes, including WNK2, TNFSF8, and IL21R, had methylation patterns inverted relative to the typical expression pattern (i.e. low methylation with high expression). Similarly, among 633 differentially methylated promoters, several including TCF3 and WNK2 demonstrated the same inverted methylation pattern. CpG islands showed distinct patterns of methylation in both subgroups that were inversely associated with expression, this also included genes differentially expressed between DHITsig+ and DHITsig- tumors. The DHITsig- group had increased levels of methylation of DHITsig genes in both promoters and gene bodies suggesting a functional role for gene body methylation. Finally, we observed that a high density of mutations near the BCL2 transcription start site consistently phased into the same haplotype as the BCL2-IGH translocation in five tumours, demonstrating the allele specificity of aSHM associated with these events (Panel B). Conclusions These results demonstrate differences in methylation between the subgroups. The association of hypomethylated superenhancers, promoters, and CpG islands with genes over-expressed in DHITsig+ suggests these methylation patterns may contribute to the DHITsig phenotype. These results may aid in improving GCB DLBCL patient classification and reveal factors contributing to its heterogeneity. Figure 1View largeDownload PPTFigure 1View largeDownload PPT Close modal

Sr ISOTOPES BY LA-MC-ICP-MS PROCEDURES COUPLED WITH THE MACS3 REFERENCE MATERIAL IN A CORAL SAMPLE: A RECORD OF ENVIRONMENTAL CHANGES

The main aim of this work is to demonstrate that the Laser ablation multi-collector inductively coupled plasma mass spectrometry (LA-MC-ICP-MS) is a powerful tool for the analysis of strontium (Sr) isotopes in corals. This work discusses certification strategies for Sr isotopes determination, using reference material (RM) analyses and the results treatment based on detailed data acquired in biological materials, a coral sample. To obtain reliable results, it is essential to properly adjust the mass spectrometer and laser ablation system. Adjusting the equipment to its maximum intensity does not always result in correct 87Sr/86Sr ratios. Therefore, the optimization of the mass spectrometer was performed using the reference material NIST SRM-987 (solution) and adjusting the correct Sr isotope ratio to the reference material (USGS MACS3 and NIST-612, solids) before each analytical session. The protocol applied the solid reference material USGS MACS3 with an isotopic ratio 87Sr/86Sr of 0.72000. The values obtained for this RM varied between 0.7012 and 0.7014, with a correction factor calculated between 0.990 and 0.988. In order to account for potential drifts in the mass spectrometer during an analytical session, the application of bracketing correction and the use of the most convenient reference material are suggested. The analytical uncertainty of Sr data obtained by LA-MC-ICP-MS is comparable to studies carried out on other carbonate materials. The results of ablation techniques are reproducible within the analytical error, which implies that this technique produces robust results when applied to coral carbonates. In addition, several comparative measurements of different reference materials (e.g. USGS MACS3 and NIST 612) and the comparison of the 87Sr/86Sr ratios highlight the robustness of the method. The results along the coral growth axes showed a decrease in the 87Sr/86Sr ratio from the inner to the outer layer of the coral (from 0.70920 to 0.70627), which indicate variations in the availability of particulate matter during the coral growth, probably related to local marine environmental changes.

Cretaceous magmatism in the Antarctic Peninsula and its tectonic implications

Periods of cessation, resumption and enhanced arc activity are recorded in the Cretaceous igneous rocks of the Antarctic Peninsula. We present new geochronological (laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS) zircon U–Pb) analyses of 36 intrusive and volcanic Cretaceous rocks, along with LA-ICP-MS apatite U–Pb analyses (a medium-temperature thermochronometer) of 28 Triassic–Cretaceous igneous rocks of the Antarctic Peninsula. These are complemented by new zircon Hf isotope data along with whole-rock geochemistry and isotope (Nd, Sr and Pb) data. Our results indicate that the Cretaceous igneous rocks of the Antarctic Peninsula have geochemical signatures consistent with a continental arc setting and were formed during the interval c. 140–79 Ma, whereas the main peak of magmatism occurred during c. 118–110 Ma. Trends in ε Hf t (zircon) combined with elevated heat flow that remagnetized rocks and reset apatite U–Pb ages suggest that Cretaceous magmatism formed within a prevailing extensional setting that was punctuated by periods of compression. A noteworthy compressive period probably occurred during c. 147–128 Ma, triggered by the westward migration of South America during opening of the South Atlantic Ocean. Cretaceous arc rocks that crystallized during c. 140–100 Ma define a belt that extends from southeastern Palmer Land to the west coast of Graham Land. This geographical distribution could be explained by (1) a flat slab with east-dipping subduction of the Phoenix Plate, or (2) west-dipping subduction of the lithosphere of the Weddell Sea, or (3) an allochthonous origin for the rocks of Alexander Island. A better understanding of the geological history of the pre-Cretaceous rocks of Alexander Island and the inaccessible area of the southern Weddell Sea is required. Supplementary material: A description of the methods used in this study and the complete dataset are available at https://doi.org/10.6084/m9.figshare.c.6089274

Experimental Study of Beam Stability Factor of Sawn Lumber Subjected to Concentrated Bending Loads at Several Points

The beam stability factor (CL) is applied in construction practices to adjust the reference bending design value (Fb) of sawn lumber to consider the lateral-torsional buckling. Bending tests were carried out on 272 specimens of four wood species, namely, red meranti (Shorea sp.), mahogany (Swietenia sp.), pine (Pinus sp.), and agathis (Agathis sp.), to analyze a simply supported beam subjected to concentrated loads at several points. The empirical CL value is a ratio of the modulus of rupture (SR) of a specimen to the average SR of the standard-size specimens. The non-linear regression estimated the Euler buckling coefficient for sawn lumber beam (KbE) in this study as 0.413, with 5% lower and 5% upper values of 0.338 and 0.488. Applying the 2.74 factor, which represents an approximately 5% lower exclusion value on the pure bending modulus of elasticity (Emin) and a factor of safety, the adjusted Euler buckling coefficient (KbE′) value for a timber beam was 1.13 (0.92–1.34), which is within the range approved by the NDS (KbE′ = 1.20). This study harmonizes the NDS design practices of CL computation with the empirical results. Because agathis has the lowest ductility (μ), most natural defects (smallest strength ratio, S), and highest E/SR ratio, the agathis beam did not twist during the bending test; instead, it failed before twisting could occur, indicating inelastic material failure. Meanwhile the other specimens (pinus, mahogany, and red meranti), which have smaller E/SR ratio, higher ductility, and less natural defects, tended to fail because of lesser beam stability. This phenomenon resulted in the CL curve of agathis being the highest among the others. The CL value is mathematically related to the beam slenderness ratio (RB) and the E/SR ratio. Because the strength ratio (S) and ductility ratio (μ) have significant inverse correlations with the E/SR ratio, they are correlated with the CL value. Applying the CL value to adjust the characteristic bending strength is safe and reliable, as less than 5% of the specimens’ SR data points lie below the curve of the adjusted characteristics values.

Time reversal invariant single-gap superconductivity with upper critical field larger than the Pauli limit in NbIr2B2

Recently, compounds with noncentrosymmetric crystal structure have attracted much attention for providing a rich playground in search for unconventional superconductivity. NbIr$_2$B$_2$ is a new member to this class of materials harboring superconductivity below $T_{\rm c} = 7.3(2)$~K and very high upper critical field that exceeds Pauli limit. Here we report on muon spin rotation ($\mu$SR) experiments probing the temperature and field dependence of effective magnetic penetration depth in this compound. Our transverse-field -$\mu$SR results suggest a fully gaped $s$-wave superconductvity. Further, the estimated high value of upper critical field is also supplemented by high field transport measurements. Remarkably, the ratio $T_{\rm c}$/$\lambda^{-2}(0)$ obtained for NbIr$_2$B$_2$ ($\sim$2) is comparable to those of unconventional superconductors. Zero-field $\mu$SR data reveals no significant change in the muon spin relaxation rate above and below $T_{\rm c}$, evincing that time-reversal symmetry is preserved in the superconducting state. The presented results will stimulate theoretical investigations to obtain a microscopic understanding of the origin of superconductivity with preserved time reversal symmetry in this unique noncentrosymmetric system.

Dust sources in Westernmost Asia have a different geochemical fingerprint to those in the Sahara

Dust is an important component of Earth's climate system, directly affecting the global radiation budget and hydrological cycle. The interaction of aerosols with clouds and its impact on regional and global energy budgets remains one of the largest sources of uncertainty in climate model predictions. Records of terrigenous dust accumulation in geological archives also provide a potentially powerful way to assess past changes in hydroclimate. Western Asia, including the Arabian Peninsula, is second only to the Saharan Desert in contributing dust to the global atmosphere. Yet, while satellite-derived maps of dust source activation frequency (DSAF) provide an increasingly granular understanding of the different dust sources within these regions today, our ability to fingerprint their windblown contributions to geological archives is rudimentary, severely limiting the use of dust-based records to reconstruct past changes in continental hydroclimate. A main limitation is a poor understanding of the mineralogical and geochemical composition of the bedrock geology and, more importantly, of the readily deflated unconsolidated sediments in these regions. Here we use published data to produce a DSAF map, centred on the Arabian Peninsula and extending from North Africa to Western Asia (∼40-10 °N; ∼25–65 °E), and we present new radiogenic isotope (Sr and Nd) data from unconsolidated surface sediment samples at active dust-producing sites. We combine our new Sr and Nd data with sparse data on sediments from the literature and the DSAF data to define three new preferential dust source areas (PSAs) in Westernmost Asia: (i) the central belt of the Arabian Peninsula, (ii) the Southern Levant and (iii) Mesopotamia. All three of these PSAs are geochemically distinct from Saharan dust sources. Long-range sediment transport by the Blue Nile and its tributaries, and the Tigris-Euphrates river systems exerts a strong influence on the geochemical fingerprints of dust sources in the Eastern Sahara and Mesopotamia, respectively. The isotopic signature of active dust sources in the central belt of the Arabian Peninsula shows only modest correspondence to underlying bedrock geology suggesting wide scale mixing by aeolian transport internally and/or a weak imprint of palaeo humidity (e.g. localized river reactivation) on dust source composition in comparison to the Eastern Sahara. Our results provide surer foundations for fingerprinting the sources of continental dust accumulating in marine, lacustrine, speleothem and ice archives, an important step in improving our understanding of Quaternary rainfall climate in arguably the most water-stressed region on Earth.

High-precision Sr and Nd isotope measurements using a dynamic zoom lens-equipped thermal ionisation mass spectrometer

Techniques for the determination of radiogenic strontium (87Sr/86Sr) and neodymium (143Nd/144Nd) isotope ratios by Thermal Ionisation Mass Spectrometry (TIMS) are presented in this study. We have developed a 5 lines acquisition routine for both elements, taking advantage of the 16 Faraday cups available on the Nu Instruments TIMS in conjunction with an efficient zoom lens system. This allows increased flexibility regarding the number of lines in a multidynamic acquisition routine whilst maintaining optimal peak alignment and peak shape for every measurement line despite the fact that the detectors are not movable. The long-term reproducibility obtained for our Sr (NBS 987) and Nd (Rennes-Ames) standard solutions gives a (87Sr/86Sr)multidyn of 0.7102467 ± 0.0000043 (6.0 ppm, 2 s.d., n = 38) and a (143Nd/144Nd)multidyn of 0.5119537 ± 0.0000022 (4.2 ppm, 2 s.d., n = 31), respectively. We also report (87Sr/86Sr)multidyn and (143Nd/144Nd)multidyn for a set of terrestrial rock standards (including 5 basalts (BCR-2, BHVO-2, BIR-1, Be-N and BR-24), one rhyolite (RGM-1) and one andesite (AGV-2)) with the same, or greater, level of precision as for the pure standards solutions. This level of precision is 2 to 3 times better than the literature data for Sr isotope ratios, and comparable to the latest high precision data reported for Nd isotope ratios. This is the first paper reporting such high precisions for radiogenic Sr and Nd data generated using a TIMS from Nu Instruments. Significant statementHigh precision Sr and Nd isotopic measurements are of key importance in the field of Earth Sciences because they are powerful tools to trace sources of materials and to date them. Here, we report the first high-precision data for 87Sr/86Sr and 143Nd/144Nd (external error of 5–6 ppm for Sr and 4–5 ppm for Nd) measured using a Nu Instruments TIMS. Such precisions will open new opportunities in fields such as geochemistry, geochronology, cosmochemistry, archaeology or forensics.

Lithological fabric as a proxy for Rb–Sr isotopic complexity

In situ Rb–Sr dating, made possible by recent analytical advancement, is a powerful chronometer that enables the timing of crystal growth or cooling to be determined for fabric forming minerals (e.g. alkali feldspar, muscovite, biotite). In contrast with accessory phase geochronology, Rb–Sr geochronology can be deployed on minerals that constitute a significant component of a wide range of rock types. Here we report laser ablation inductively coupled plasma tandem mass spectrometry (LA-ICP-MS/MS) biotite Rb–Sr ratios in metaigneous and metasedimentary samples from across Western Australia. These biotite samples span a diversity of structural, metamorphic, and temporal states, yet highlight common salient features of this chronometer. Biotite in these samples received its isotopic compositions from completely to partially homogenized Sr reservoirs, as evident from isochronous to more complex distributions of isotopic ratios. The utility of the classic isochron approach is contrasted with biotite model ages for the geologic interpretation of Rb–Sr results for samples with and without constrained initial 87Sr/86Sr ratio. Model ages calculated from individual analyses aid in identifying multiple discrete events that may have only partially equilibrated isotopic systems. Thus, single-analysis model ages can enable the extraction of thermochronological information from complex Rb–Sr data sets, if interpreted under consideration of their geologic context. Textural analysis of thin sections via Fourier component image analysis quantifies the preferred orientation of biotite fabrics. This analysis reveals a correlation between diversity of grain orientation and biotite age complexity. Such a simple texture-to-age relationship highlights a potential pre-analysis screening tool to facilitate sample selection where Rb–Sr isochrons are sought.Results reveal a thermal event at ca. 550–500 Ma in the Lamboo Province, West Kimberley, and multiple contact metamorphic events at ca. 633 Ma and 619–615 Ma that occurred in the Yeneena Basin, Paterson Orogen. Biotite from the Yilgarn Craton yields a strong E-W trend in cooling ages, from 2477 Ma in the central Yilgarn Craton to 580 Ma at the western margin of the craton. These ages support slow cooling and thermo-tectonic quiescence after cratonisation in the central Yilgarn Craton, while the western margin was subject to Neoproterozoic reworking. Placed into a regional geologic context, these results highlight the sensitivity of the in situ Rb–Sr dating method to constrain the timing of geologic events that are not commonly captured by other isotopic systems.

Calcium Isotopic Constraints on the Transition From Aragonite Seas to Calcite Seas in the Cambrian

AbstractThe primary mineralogy of marine carbonates has varied over geological time in concert with the secular evolution of global climate and seawater chemistry. Here, we employed a multi‐proxy geochemical and petrographic approach, including measuring the Ca isotope (δ44Ca) and Sr content of Ediacaran–Cambrian carbonates, to provide new insights into the timing of the transition from a “dolomite‐aragonite sea” to a “calcite sea” across the Ediacaran‐Cambrian transition. We find robust evidence for the persistence of an aragonite sea well into Cambrian Age 2 (and potentially up through Age 4). Together with an updated petrographic compilation of abiotic carbonate precipitates (i.e., ooids and cements), these new δ44Ca and Sr data provide further evidence that there was a protracted transition from aragonite seas to calcite seas in the Cambrian. We propose that this transition was mediated, in part, by changes in seawater Mg/Ca ratios potentially regulated by the global marine redox state and extents of authigenic clay precipitation.

Field Data Collection Methods Strongly Affect Satellite-Based Crop Yield Estimation

Crop yield estimation from satellite data requires field observations to fit and evaluate predictive models. However, it is not clear how much field data collection methods matter for predictive performance. To evaluate this, we used maize yield estimates obtained with seven field methods (two farmer estimates, two point transects, and three crop cut methods) and the “true yield” measured from a full-field harvest for 196 fields in three districts in Ethiopia in 2019. We used a combination of nine vegetation indices and five temporal aggregation methods for the growing season from Sentinel-2 SR data as yield predictors in the linear regression and Random Forest models. Crop-cut-based models had the highest model fit and accuracy, similar to that of full-field-harvest-based models. When the farmer estimates were used as the training data, the prediction gain was negligible, indicating very little advantage to using remote sensing to predict yield when the training data quality is low. Our results suggest that remote sensing models to estimate crop yield should be fit with data from crop cuts or comparable high-quality measurements, which give better prediction results than low-quality training data sets, even when much larger numbers of such observations are available.

Monitoring Optical Variability in Complex Inland Waters Using Satellite Remote Sensing Data

Optical classification for water bodies was carried out based on satellite remote sensing data, which avoided the limitation of having a limited amount of in situ measured spectral data. Unsupervised cluster analysis was performed on 53,815 reflectance spectra extracted at 500-m intervals based on the same season or quasi-same season Landsat 8 SR data using the algorithm of fuzzy c-means. Lakes and reservoirs in the study area were comprehensively identified as three optical types representing different limnological features. The shape and amplitude characteristics of the reflectance spectra for the three optical water types indicated that one corresponds to the clearest water, one corresponds to turbid water, and the other is moderate clear water. The novelty detection technique was further used to label the match-ups of the in situ data set collected during 2006 to 2019 in 12 field surveys based on mathematical rules of the three optical water types. The results confirmed that each optical water type was associated with different bio-optical properties, and the total suspended matter of the clearest, moderate clear and turbid water types were 14.99 mg/L, 41.06 mg/L and 83.81 mg/L, respectively. Overall, the clearest, moderate clear and turbid waters in the study area accounted for 49.3%, 36.7% and 14.0%, respectively. The spatial distribution of optical water types in the study area was seamlessly mapped. Results showed that the bio-optical conditions of the water distributed across the southeast region were roughly homogeneous, but in most of other regions and within some water bodies, they showed a patchy distribution and heterogeneity. This study is useful for monitoring water quality and provides a useful foundation to develop or tuning algorithms to retrieve water quality parameters.

Metamorphism of the Korvatundra Structure of the Lapland–Kola Orogen (Arctic Zone of the Fennoscandian Shield)

AbstractWe study the P–T conditions and age of metamorphic evolution of the rocks that make up the Korvatundra structure in the northeast of the Fennoscandian Shield. The rocks underwent progressive metamorphism of the amphibolite facies at 625–660 ºC and 8.7–8.8 kbar 1945 ± 34 Ma (Sm–Nd data). The pegmatite cutting the metamorphic paragenesis that formed at this stage has an age of 1917 ± 6 Ma (zircon U–Pb data). Metamorphic transformations after 1917 Ma are manifested locally as discrete zones of blastomylonites in the rocks of the northern part and some inner sites of the Korvatundra structure. Both local increases and decreases in temperature and pressure are possible in these zones. The formation of light titanite with an age of 1863 ± 44 Ma marks the next stage of shear strain. Low-temperature alterations (chloritization and silicification) took place in the zones of final deformations 1722 ± 5 Ma (Rb–Sr data). Beginning from 1.94 Ga, the general deformational and metamorphic history of the Korvatundra structure, Lapland Granulite Belt, and Tana Belt confirms the assumption of the formation of a single inverted metamorphic zoning within the Korvatundra structure and the overlying Lapland–Kolvitsa Collision Belt in the Paleoproterozoic. The obtained data supplement the idea of the Paleoproterozoic geodynamic evolution of the Lapland–Kola orogen.

Inelastic Processes in Strontium-Hydrogen Collisions and Their Impact on Non-LTE Calculations

Inelastic processes rate coefficients for low-energy Sr + H, Sr+ + H−, Sr+ + H, and Sr2+ + H− collisions are calculated using the multichannel quantum model approach. A total of 31 scattering channels of SrH+ and 17 scattering channels of SrH are considered. The partial cross sections and the partial rate coefficients are hence calculated for 1202 partial processes in total. Using new quantum data for Sr ii + H i collisions, we updated the model atom of Sr ii and performed the non-local thermodynamic equilibrium (non-LTE) calculations. We provide the non-LTE abundance corrections for the Sr ii resonance lines in two grids of model atmospheres, which are applicable to very metal-poor ([Fe/H] ≤−2) dwarfs and giants.

Spatio-Temporal Extraction of Surface Waterbody and Its Response of Extreme Climate along the Upper Huaihe River

The upper Huaihe River is the water-producing area of the Huaihe River Basin and the major grain and oil-producing area in China. The changing global climate over the recent years has increased the frequency of extreme weather in the upper reaches of the Huaihe River. Research on the responses of surface water bodies to extreme climates has become increasingly important. Based on all utilizable Landsat 4–8 T1–SR data and frequency mapping, the spatio-temporal extraction of surface water and its response to extreme climate were studied. We generated high-precision frequency maps of surface water, and a comparison of cartographic accuracy evaluation indices and spatial consistency was also carried out. The high-precision interpretation of small waterbodies constructs a surface water distribution with better continuity and integrity. Furthermore, we investigated the effect of El Niño/La Niña events on precipitation, temperature, and surface water along the upper Huaihe River, using the Mann–Kendall mutation tests. The results show: in 1987–2018, periods of abrupt changes in precipitation coincide with EI Niño/La Niña events, indicating that the precipitation was sensitive to EI Niño/La Niña events, which also strongly correlated with surface water area during wet and dry years. The effect of extreme events on seasonal water was smaller than permanent water. Surface water area showed an insignificant declining trend after 1999 and a significant drop in 2012. The phenomenon of topographic enhancement of precipitation controlled the spatial distribution of permanent water, with human activities having a substantial effect on the landscape pattern of seasonal water. Finally, discussions and applications related to the Markov Chain probability calculation theory in the paper contributed to enriching the theories on frequency mapping. The relevant results provide a theoretical basis and case support for the formulation of long-term water resources utilization and allocation policies.

Blood profile of Tilapia (Oreochromis niloticus) fed fortification feed with seaweed flour (Gracilaria sp.)

Seaweed Gracilaria sp. is a marine plant that contains secondary metabolites that can be used as an immunostimulant in tilapia (Oreochromis niloticus). The blood picture can be used as an evaluation material for the physiological response of fish. The aim of the study was to determine the effect of fortification of seaweed flour Gracilaria sp. on the blood profile of tilapia. The study used an experimental method with 4 treatments, namely, P1: control feed; P2: flour fortification of Gracilaria sp. 4%; P3: 8%; and P4: 12% respectively. The research data were analyzed by linear regression for the blood profile and variance for the absolute weight, SR, and FCR data. The results showed that fortification of seaweed flour Gracilaria sp. the feed did not have a significant effect on hemoglobin levels, hematocrit, erythrocyte counts, and leukocytes. However, it has a significant effect on increasing absolute weight, survival, and feed conversion rates. Flour fortification of Gracilaria sp. with a concentration of 8% or 80g/kg of feed is the best concentration that can affect the blood profile