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101.
102.
E. M. Gichangi M. Gatheru E. N. Njiru E. O. Mungube J. M. Wambua J. W. Wamuongo 《Climatic change》2015,130(2):287-297
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Data on the ion-salt, microcomponent, gas, microbiological, and isotopic composition of water and the results of studies of
the equilibriums in the water-rock system are used to analyze the formation processes of the composition of Tersinskie carbonic-acid
mineral water and their genesis. 相似文献
106.
Doklady Earth Sciences - The results of the first observations of mode 2 internal waves in the Black Sea are presented. The measurements were carried out on the Crimean shelf from the MGI platform... 相似文献
107.
Kozoderov V. V. Kondranin T. V. Dmitriev E. V. 《Izvestiya Atmospheric and Oceanic Physics》2017,53(9):1132-1141
Izvestiya, Atmospheric and Oceanic Physics - The basic model for the recognition of natural and anthropogenic objects using their spectral and textural features is described in the problem of... 相似文献
108.
Theoretical Developments in Electromagnetic Induction Geophysics with Selected Applications in the Near Surface 总被引:4,自引:1,他引:3
Mark E. Everett 《Surveys in Geophysics》2012,33(1):29-63
Near-surface applied electromagnetic geophysics is experiencing an explosive period of growth with many innovative techniques
and applications presently emergent and others certain to be forthcoming. An attempt is made here to bring together and describe
some of the most notable advances. This is a difficult task since papers describing electromagnetic induction methods are
widely dispersed throughout the scientific literature. The traditional topics discussed herein include modeling, inversion,
heterogeneity, anisotropy, target recognition, logging, and airborne electromagnetics (EM). Several new or emerging techniques
are introduced including landmine detection, biogeophysics, interferometry, shallow-water electromagnetics, radiomagnetotellurics,
and airborne unexploded ordnance (UXO) discrimination. Representative case histories that illustrate the range of exciting
new geoscience that has been enabled by the developing techniques are presented from important application areas such as hydrogeology,
contamination, UXO and landmines, soils and agriculture, archeology, and hazards and climate. 相似文献
109.
Saeed Kiaalhosseini Richard L. Johnson Richard C. Rogers Maria Irianni Renno Mark Lyverse Thomas C. Sale 《Ground Water Monitoring & Remediation》2016,36(4):41-49
We evaluated tools and methods for in situ freezing of cores in unconsolidated subsurface media. Our approach, referred to as cryogenic core collection (C3), has key aspects that include downhole circulation of liquid nitrogen (LN) via a cooling system, strategic use of thermal insulation to focus cooling into the core, and controlling LN back pressure to optimize cooling. Two cooling systems (copper coil and dual‐wall cylinder) are described. For both systems, the time to freeze a single 2.5‐foot (76‐cm) long by 2.5‐inch (63‐mm) diameter core is 5 to 7 min. Frozen core collection rates of about 30 feet/day (10 m/day) were achieved at two field sites, one impacted by petroleum‐based light nonaqueous phase liquids (LNAPLs) and the other by chlorinated solvents. Merits of C3 include (1) improved core recovery, (2) potential control of flowing sand, and (3) improved preservation of critical sediment attributes. Development of the C3 method creates novel opportunities to characterize sediment with respect to physical, chemical, and biological properties. For example, we were able to resolve water, LNAPL, and gas saturations above and below the water table. By eliminating drainage of water, gas and LNAPL saturations in the range of 6 to 23% and 1 to 3% of pore space, respectively, were measured in LNAPL‐impacted intervals below the water table. 相似文献
110.
S.?V.?VyatkinEmail author G.?Yu.?Kriulina V.?K.?Garanin D.?G.?Koshchug E.?A.?Vasilyev 《Moscow University Geology Bulletin》2018,73(2):161-165
Two samplings of 65 diamond crystals divided by the intensity of a slow X-ray luminescence component are studied from the Arkhangel’skaya and Karpinskogo-1 pipes. IR and EPR spectroscopies revealed a relationship between the nitrogen A and P2 centers of the diamonds and the presence of a slow X-ray luminescence component. Its absence in most diamonds with high content of P1 (C) centers is explained by the low number of A and P2 centers. 相似文献