Geochemical distribution and genesis of selenium-rich soils in Maojie Town on the Yunnan low-selenium belt. [PDF]
Dong C +5 more
europepmc +1 more source
Characterization and source apportionment of heavy metal contamination in agricultural soils in the complex genesis region of western Yunnan. [PDF]
Li Y +9 more
europepmc +1 more source
Physicochemical characterization and industrial use of Awzet Kaolin deposit in Northwestern Ethiopian plateau. [PDF]
Ali MY.
europepmc +1 more source
Decontaminating Solar Wind Samples with the Genesis Ultra-Pure Water Megasonic Wafer Spin Cleaner [PDF]
The Genesis sample return capsule, though broken during the landing impact, contained most of the shattered ultra-pure solar wind collectors comprised of silicon and other semiconductor wafers materials.
Allton, J. H. +3 more
core +1 more source
On the reasons and quantified prevalent ocean atmosphere roles for the intensification and genesis features of the ESCS Tauktae. [PDF]
G G Z, R H.
europepmc +1 more source
Editorial: Mineral solubilizing microorganisms (MSM) and their applications in nutrient bioavailability, bioweathering and bioremediation, volume III. [PDF]
Mumtaz MZ, Ahmad M, Mustafa A.
europepmc +1 more source
Differential Responses of Invasive Trees <i>Ailanthus altissima</i> Mill. Swingle and <i>Fraxinus americana</i> L. to Soil Phosphorus Availability. [PDF]
Milutinović M +5 more
europepmc +1 more source
Environmental Stressors and Cardiovascular Health: Acting Locally for Global Impact in a Changing World: A statement of the European Society of Cardiology, the American College of Cardiology, the American Heart Association, the World Heart Federation. [PDF]
Münzel T +5 more
europepmc +1 more source
Genome Sequence of the Cluster EF Bacteriophage TinyMiny, Isolated using <i>Microbacterium foliorum</i>. [PDF]
Duffy I +14 more
europepmc +1 more source
Soil genesis in recently deglaciated areas [PDF]
Climate change has huge impacts on mountain ecosystems. One visible effect is glacier retreat, which has continued with only few interruptions since the end of the Little Ice Age (LIA), around the mid-nineteenth century. The released surfaces in the proglacial areas (glacier forefields) offer the opportunity to observe the development of soil ...
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