Evaporation from rocks is a poorly understood, yet important process. In the recent study, an evaporation rate from 10 lithologies, including sedimentary, igneous, and metamorphic granular rocks, was measured and calculated. The measured evaporation rate varied over four orders of magnitude (0.4–2447 mm/year), and the calculations reasonably followed the measured values. Within the range of observed values, the evaporation rate was mostly influenced by the vaporization plane depth below the rock surface (by up to 2.2 orders of magnitude), which was followed by: lithology (up to 1.1 order of magnitude), local climate (up to 1.0 order of magnitude), and climate seasonality (up to 0.8 order of magnitude). Thus, our study shows the key role of the vaporization plane depth in the evaporation rate. This approach can find employment in a large number of investigations such as in the evaporation estimates and hydrologic balance in rock landforms and rocky slopes, hydrologic processes in the shallow rock subsurface, living conditions of endolithic and epilithic organisms, weathering processes, and in the protection of carved or rock constructed cultural heritage.

Slavík M., Bruthans J., Schweigstillová J. (2018): Evaporation rate from surfaces of various granular rocks: Comparison of measured and calculated values. Science of the Total Environment 856, 159114. (DOI)

Diachronous opening of the Rheic Ocean and separation of Avalonian–Cadomian terranes from Gondwana was a major, but still poorly understood paleogeographic event in the late Ediacaran to early Cambrian. A recent study from the Příbram–Jince basin in the Bohemian Massif revealed a significant provenance and paleocurrent changes in response to dextral transtension that enlarged the basin into a pull-apart structure, suggesting that strike-slip movements along the former Avalonian–Cadomian belt controlled the diachronous opening of the Rheic Ocean. Putting this piece of information into a plate-tectonic picture, it seems that an inherited suture in the Avalonian ribbon terrane facilitated complete rifting and rift–drift transition while the Cadomian terranes, including those now forming the Bohemian Massif, remained attached to Gondwana during this large-scale rifting event.

Syahputra R., Žák J., Nance R.D. (2021): Cambrian sedimentary basins of northern Gondwana as geodynamic markers of incipient opening of the Rheic Ocean. Gondwana Research 105, 492-513. (DOI)

Cobalt is one of the most important critical metals which could be potentially extracted from the old metallurgical slags in the Zambian Copperbelt. The slags from Luanshya, the oldest mining and smelting site in the Copperbelt, contain up to 5990 ppm Co (median: 2370 ppm). The detailed mineralogical investigation combined with the sulfuric acid leaching simulating hydrometallurgical recovery indicated that up to 67% of Co can be extracted from slag in a short period of time (24 h). However, despite the dramatic increase of Co prices on the global market, its recovery from the Luanshya slags appears to be non-economical due to the high costs of the mechanical and chemical processing of the slag materials. The paper is freely available via open access:

Ettler V., Mihaljevič M., Drahota P., Kříbek B., Nyambe I., Vaněk A., Penížek V., Sracek O., Natherová V. (2022): Cobalt-bearing copper slags from Luanshya (Zambian Copperbelt): Mineralogy, geochemistry, and potential recovery of critical metals. Journal of Geochemical Exploration 237, 106987. (DOI)

We compared analogous healthy topsoils and ones burned by fires of different temperatures for their elemental and isotopic Pb content. The fires only affected the top 5 cm of the soil. We found that soils affected by low-temperature fires had increased Pb compared to healthy soils. The accumulation of Pb was not observed in the soils exposed to higher temperatures. The same results were found in ash. Lead isotopic ratios were affected by the fires. These increased in soils affected by higher temperatures but didn’t change with the low temperatures. We proposed that the temperature dependence is due to anthropogenic Pb (²⁰⁶Pb/²⁰⁷Pb < 1.16) volatilizing at lower temperatures than geogenic Pb (²⁰⁶Pb/²⁰⁷Pb > 1.19). This work suggests that it may be possible to determine the temperature of a forest fire from the Pb isotopic signatures of the burned materials.

Baieta R., Vieira A.M.D, Vaňková M., Mihaljevič M. (2022). Effects of forest fires on soil lead elemental contents and isotopic ratios. Geoderma 414, 115760. (DOI)