On the estimation of volume of strain in earthquakes

Summary A relation between the volume of strain and the area of faulting in earthquakes has been derived. An empirical linear relationship between the magnitudeM of an earthquake and the logarithm of the volume of strainV has been obtained using data from 20 earthquakes.     

UTCHEM model application for prediction of crude oil removal from contaminated sand columns

Soil pollution by crude oil is a challenging environmental issue for oil producing countries. Several methods have been developed for remediation of the contaminated soil including washing with different detergents. In this work, we applied UTCHEM simulator model to the sand columns polluted by 10000 and 30000 ppm of crude oil which was treated with 0.05, 0.1 and 0.2 wt% of a biological detergent, saponin. The results showed a good agreement between simulated and pilot study. The maximum remediation was 61% with a pH of 9 when we utilized 0.2 wt% saponin for the column contaminated with 30000 ppm of crude oil. 47% remediation was achieved with a pH of 9 when 0.1wt% of detergent was applied to the same column. Sensitivity analysis indicated an increase in remediation by increasing the pH with the optimum pH of 11. The best possible concentrations of surfactant solutions were 0.1 and 0.2 wt% for 10000 and 30000 ppm pollution, respectively, resulting in crude oil removal efficiencies of 69% and 72%, respectively. Simulation results also indicated that an increase in the permeability of the sand columns would also result in an increased remediation.     

Structural parageneses in a discrete geological medium

The theoretical bases of the structural-paragenetic method for the reconstruction of geodynamic environments are critically analyzed in view of ideas about nonlinear dynamics and the coarse discrete fractality of the geological medium. The work shows the incorrectness of reconstructions without considering bifurcations of structurization and its strong dependence on differences in initial conditions, the unreliability of recognizing particular parageneses of different ages, types, and ranks, as well as that without immediate observational and experimental examination of the conformity of reconstructions to the real environments of the geological past.     

Change in the circulation regime in the stratified saline Lake Shira (Siberia,Republic of Khakassia)

The in-situ data on the vertical structure and stability of the vertical stratification of saline Lake Shira over the past decade (2007–2015) are analyzed. Simplified mathematical models have shown that strong wind in the autumn of 2014 together with rather thick ice in the winter of 2015 caused a change in the circulation regime of this water reservoir from meromictic (incomplete mixing) to holomictic (compete mixing). Based on the results obtained, a circulation regime for deep saline lakes located in the continental climate zone, in particular, in the arid zones of Southern Siberia (Khakassia, Transbaikal, and Altai) can be predicted under various climate scenarios of the future.     

Case study of Pampa,Texas, multicell storms

Analysis of the Pampa, Texas, multicell storms showed prestorm environmental conditions of a strong horizontal convergence of moisture, mixing ratio 12 g/kg at the 850 mb level in the Texas Panhandle areas and strong winds with shear veering with height. Rapid-scan satellite imagery showed that the clouds penetrated above the tropopause and cloud-top temperatures were at least 4 to 9° C colder than the temperature of the tropopause. This formation and collapsing of high-mass-density overshooting cloud tops above the tropopause is characteristic of tornadoes in the middle portion of the United States.     

Localised coherent response of the La Molina basin (Lima,Peru) to earthquakes,and future approaches suggested by Parkway basin (New Zealand) experience

Earthquake records from a 1984 temporary seismograph array set up in La Molina, Lima, Peru, are re-analysed. The array comprised eight three-component geophones; seven soil based and one rock based. Values of horizontal-to-vertical spectral ratio (HVSR) for two small earthquakes peaked at around 1.3 Hz. In one distant earthquake, four of the seven soil-based stations showed a peak at 1.25 Hz in soil-to-rock spectral ratio (SSR), the same dominant frequency observed during an aftershock of a damaging earthquake. Because this frequency is not compatible with the shear wave velocity profile attributed to La Molina, and because the spectral peak is confined to a small ground area, it is concluded that the peak is caused by a localised deposit of soft soil. Because the area associated with the spectral peak includes the area of great damage in 1974, it is concluded that coherent monochromatic behaviour is responsible for the damage.     

Higher anthraxolites

Recent years have been marked by progress in studying the structure of natural X-ray amorphous substances, anthraxolites included, by scanning electron and atomic power microscopy. Integration of the available data on molecular and supramolecular structure of higher anthraxolites from Karelia, Novaya Zemlya, and the Urals allowed elaboration of new classification criteria for solid bitumen, namely, degree of structure perfection and micromineral composition. This approach will help to eliminate disadvantages of traditional investigation of solid bitumen.     

Cargo spillage at an iron ore unloading terminal

Dust deposition in the sea at an iron ore unloading terminal in the Firth of Clyde, Scotland, was measured by means of sediment collectors placed 10 m above the sea bed on the outer face of the unloading jetty. A ‘background’ sedimentation of up to 64 g m^?2 day^?1 of non-ferrous material was obtained with no ships in port. During unloading dust quantities up to 18 021 g m^?2 day^?1 were obtained, but the quantities depended on the type of ore unloaded, and much smaller quantities of sediment were obtained with ores less prone to fine particle formation. Any ecological effects would involve sea bed benthos, although rates of transportation of the sedimented dust are probably rapid in the immediate vicinity of the ore terminal.