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This conclusion is supported by the lower maximum Al and Fe concentrations (Table 1) as indicator of quick surface water intrusion in most of the springs compared to subsurface rivers.
This interface, having different chemical, physical and biological properties compared to subsurface waters, plays a significant role in biogeochemical processes on a global scale (i.e., air sea gas exchange, trace gas deposition to the ocean, and secondary organic aerosol formation).
Approximately 35 45% of equivalent soil mass SOC stocks were distributed in the upper soil layer (0 20 cm) in stands of all ages, indicating more organic C accumulation in the surface layer compared to subsurface layers (> 20 cm).
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Overall, the genome sequence of G. bemidjiensis offers surprising insights into the metabolism and physiology of Geobacteraceae in subsurface environments, compared to non-subsurface Geobacter species, such as the ability to disproportionate fumarate, more efficient oxidation of propionate, enhanced responses to oxygen stress, and dependence on the environment for a vitamin requirement.
However, the Sehkaniyan Formation displays lower acoustic velocity for a given porosity at outcrop compared to the subsurface.
Although the sputter yield of Au is ten times that of Si, we speculate the dominant Au concentration at the top 1-2 monolalong (along the surface nanostructures) compared to the subsurface which is likely due to the ion-induced segregation mechanism since the gold surface tension is known to be lower than Si.
Based on our study, spring and well water seems to be most suitable for the installation of groundwater extraction facilities because of the relatively constant hydrochemistry and low turbidity compared to surface and subsurface rivers.
This study examines whether there are significant differences in the metabolism and physiology of G. bemidjiensis compared to non-subsurface Geobacter species.
On average, the mineralization of all springs (2009: 543 ± 76 µS/cm) is higher compared to surface and subsurface river waters and more or less constant over all seasons with slightly lower values during rainy season 2010.
Compared to HSSF, the subsurface vertical flow constructed wetland (SVFCW) system is more effective for the mineralization of biodegradable organic matter and has greater oxygen transport ability [ 15].
The weathered layer as compared to the other two subsurface layers or geological units exhibits the lowest range resistivity values (19 281 Ωm).
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