Resultados de investigación

Compositional analysis by PIXE of the four samples; XRD measurements of sample x = 0.21 as a representative of samples; saturation magnetization (MS) determined from magnetic measurements; obtaining the blocking-temperature distribution f(TB) from magnetization measurements as a function of temperature; magnetization measurements of CBO and paraffin without NPs at 300 K; MFH measurements of CBO and paraffin without NPs; changes in the physical aspects of CBO with temperature; cooling curve of CBO + NPs heated in a hot plate up to a temperature above the melting point and its analysis with respect to quantity Γ(t); cooling curve of paraffin with NPs heated in a hot plate up to a temperature above the melting point and its analysis with respect to quantity Γ(t); and MFH of the four samples dispersed in toluene., Peer reviewed

Fabrication, characterization, analysis, and cleaning strategies for removal of the excess recast material of metallic membranes by laser machining; synthesis and characterization details of deep eutectic solvent (DES) to be used as the dispersed phase for membrane emulsification studies; supporting details on the experimental procedure of membrane emulsification studies to characterize the produced nanoemulsions by DLS and TEM and antimicrobial susceptibility testing of the optimized emulsions., Peer reviewed

Figure S1 Relative gene expression of ALP, BSPII, and RUNX2 genes in hBM-MSCs cultured for 3 days in osteogenic condition and COLII gene for 3 days in chondrogenic condition. *** p < 0.01 as compared to PCL, Figure S2 Staining with Alkaline Phosphatase after 7 days of culture of hBM-MSCs on the two types of scaffolds (PCL and PCL-HAp) in an osteogenic medium. Bars represent 4 mm in (A,C) and 50 µm in (B,D), Figure S3 In vivo subcutaneous implantation of a sterilized scaffold for two weeks. (A,B) Macroscopic analyses showing the good integration and vascularization of the implant, (C,D) Haematoxylin-Eosin (HE) staining, yellow zone: implanted membrane; red zones: blood vessels; blue zones: immune cell aggregates; and white asterisk: fibrocytes, Figure S4 Haematoxylin-Eosin (HE) staining (a–h) and histological staining with Alizarin Red S (i–p) for PCL, PCL-HAp, PCL-HA, and PCL-HAp-HA scaffolds subcutaneously implanted for 4 weeks without cells in ICR mice. S4-1 in (a,e,i,m) for the PCL scaffold S4-2 in (b,f,j,n) for the PCL-HAp scaffold; S4-3 in (c,g,k,o) for the PCL-HA scaffold; and S4-4 in (d,h,l,p) for the PCL-HAp-HA scaffold. Black arrowheads indicate vascularization. Black squares indicate the enlarged areas., Peer reviewed

Crystallographic data (powder) of the tetragonal and orthorhombic crystal structures for La1.5Ca0.5CoO4.02. Comparison between the modulus and imaginary part of the FT of the k-weighted polarized EXAFS spectra and best fits of La1.5Ca0.5CoO4.02 for in-plane and out-of-plane configurations at room temperature and best-fit structural parameters for the second coordination shells obtained from fitted polarization-dependent k-weighted EXAFS spectra at room temperature for the La2–xAxCoO4±δ (A = Sr, Ca) single crystals., Peer reviewed

Experimental details of the synthesis protocol; characterization procedures; N-type sample characterization; and XPS details of M-type samples., Peer reviewed

1. Vector coverages (shapefiles, 1:50,000, EPSG 25830) of the distribution of eight zonal forest types in mainland Spain. The dominant species and Habitat Type code (European Habitats Directive 92/43 EEC) are: • Fagus sylvatica (9120, 9130 and 9150) • Quercus robur and Q. pyrenaica (9230) • Q. suber (9330) • Pinus uncinata (9430) • P. nigra ssp. salzmannii (9530) • P. pinea (subset of 9540) 2. R scripts to determine patchiness using the Korcak exponent B. This is computed both for the entire range of patch sizes and for size intervals using a segmented regression approach. Such intervals are automatically detected., Peer reviewed

TEM image and histograms of bare gold nanorods, UV–vis–NIR spectra of AuNRs–cellulose composites, TGA analysis results, EDS elemental maps, XPS analysis results, effect of pH on the photoregeneration of NADH, UV–vis spectra of the samples during investigations of the mechanism of cellulose-assisted photocatalysis, UV–vis spectra of the photocatalyst after each recycling cycle, and UV–vis spectra of all of the control experiments., Peer reviewed

Additional figures and tables and crystallographic data., Peer reviewed

A set of historical tide gauge sea level records from Alicante (Spanish Mediterranean coast) have been recovered from logbooks stored at the Spanish National Geographical Institute (IGN). Sea level measurements have been digitised, quality-controlled and merged into two consistent sea level time series. Vertical references among instruments benchmarks have been derived from high precision vertical levelling surveys. Earlier observations are daily averages and more recent data are hourly values. The observations are from 7 different tide gauge records in Alicante outer harbour (Alicante I) and five tide gauge series in Alicante inner harbour (Alicante II). The sea level record in Alicante starts in 1870 with daily averaged values until the 1920s and hourly afterwards, and is still in operation, thus representing the longest tide gauge sea level time series in the Mediterranean Sea. The sea level at Alicante I has been measured by tide pole, floating gauge, mechanical recorder, digital recorder and since 2014 by radar gauge. The sea level at Alicante II has been measured by floating gauge, digital recorder and from 2014 onwards by radar gauge. This scarcity of long-term sea-level observations, as well as their uneven geographical distribution is a major challenge for climate studies that address, for example, the quantification of mean sea-level rise at centennial time scales, the accurate assessment of sea-level acceleration or the long-term changes in sea-level extremes that are vital for coastal risk assessments. This dataset represents an additional effort of sea-level data archaeology and aims at preserving the historical scientific heritage that has been up to now stored in old archives in non-electronic format. The research was partially funded by the Spanish Ministry of Science, Innovation and Universities. A further series was rescued from Santander under the same initiative. These data are distributed under a CC BY 4.0 license (creativecommons.org/licenses/by/4.0/)., Peer reviewed

A set of historical tide gauge sea level records from Santander (Northern Spain) have been recovered from logbooks stored at the Spanish National Geographical Institute (IGN). Sea level measurements have been digitised, quality-controlled and merged into a consistent sea level time series. Vertical references among instruments benchmarks have been derived from high precision vertical levelling surveys. The observations were recorded as daily averages and are from three different instruments in two locations in Santander (Spain). The historical sea level record in Santander consists of a daily time series spanning the period 1876-1928 and it is further connected to the modern tide gauge station nearby, ensuring datum continuity up to the present. The data from Santander comes from a floating gauge and then syphon gauges. This scarcity of long-term sea-level observations, as well as their uneven geographical distribution is a major challenge for climate studies that address, for example, the quantification of mean sea-level rise at centennial time scales, the accurate assessment of sea-level acceleration or the long-term changes in sea-level extremes that are vital for coastal risk assessments. This dataset represents an additional effort of sea-level data archaeology and aims at preserving the historical scientific heritage that has been up to now stored in old archives in non-electronic format. The research was partially funded by the Spanish Ministry of Science, Innovation and Universities. A further two series were rescued from Alicante under the same initiative. These data are distributed under a CC BY 4.0 license (creativecommons.org/licenses/by/4.0/)., Peer reviewed