Thermal and Textural Properties of Organogels Developed by Candelilla Wax in Safflower Oil
Fluid Inclusion Studies of Chemosynthetic Carbonates: Strategy for Seeking Life on Mars
Astrobiology is a field that investigates the potential of fluid inclusions in minerals from other worlds. These inclusions are microscopic chambers that capture and preserve ambient fluids during mineral precipitation, potentially including biosignatures and physical remains of extra-terrestrial life. The researchers’ work, which centres on chemosynthetic carbonates and other surficial rock types, utilises cutting-edge technology to extract and analyse these inclusions, providing a fresh viewpoint in the field of astrobiology using a Linkam THM600 stage, the predecessor to the Linkam THMS600 stage.
Deliquescence and efflorescence of calcium perchlorate: An investigation of stable aqueous solutions relevant to Mars
The preservation of fluid inclusions in diverse surface precipitates: the potential for sampling palaeo-water from surface deposits on Mars
The Planetary Spectroscopy Laboratory (PSL): Wide spectral range, wider sample temperature range
Multi-scale thermal stability of a hard thermoplastic protein-based material
Macroscopic CNT fibres inducing non-epitaxial nucleation and orientation of semicrystalline polymers
Retardation of cold flow in immiscible rubber blends by tailoring their microstructures
Enhancement of Mechanical and Self‐Healing Performance in Multiwall Carbon Nanotube/Rubber Composites via Diels–Alder Bonding
Effect of the melting temperature on the crystallization behavior of a poly(l‐lactide)/poly(d‐lactide) equimolar mixture
Structure and Properties of Silica Glass Densified in Cold Compression and Hot Compression
A Novel Peptide Hydrogel for an Antimicrobial Bandage Contact Lens
A thermally responsive, rigid, and reversible adhesive
Read the full paper here… access required.
Microstructural change of degummed Bombyx mori silk: An in situ stretching wide-angle X-ray-scattering study
Synthesis of organic aerogels with tailorable morphology and strength by controlled solvent swelling following Hansen solubility
Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
Read More here:
Thermal expansion coefficient of few-layer MoS2 studied by temperature-dependent Raman spectroscopy
Read the full paper here:
https://www.nature.com/articles/s41598-021-86479-6
