#G OXYGEN FORENSICS MANUAL#
#G OXYGEN FORENSICS ANDROID#

Updated live and deleted data parsing from Telegram (all versions) from Android OS devices and from Telegram from iOS devices.ДЄdded support for 200+ new Android OS devices: Asus Memo Pad 7 ME572C (K007), Intex Aqua Trend, Maxwest Astro 6, Samsung Galaxy J1 Ace Duos 4G (SM-J110F/DS), Sony Mobile Xperia Z5 Premium Dual (E6883), Toshiba Excite Go (AT7-C8), etc.Д¬hanges in version 8. Added live and deleted data parsing from TomTom Russia (1.21) from iOS devices.ДЄpplications. Added live and deleted contacts parsing from TomTom GPS Navigation Traffic (1.7) from Android OS devices.ДЄpplications. Added live and deleted data parsing from Kate Mobile (23.1) from Android OS devices.ДЄpplications. Added data extraction via MTP protocol.ДЄpplications. Updated live and deleted data parsing from Odnoklassniki (5.3.0.451) from iOS devices.ДЄdded support for 150+ new mobile devices: BlackBerry PRIV (STV100-1), Gigabyte GSmart Essence 4, HTC One A9, HTC Desire 728G, Nokia Lumia 1020, Motorola Moto G 3rd Gen 2015 TD-LTE (XT1550), Oppo Neo 7, Zopo Speed 7 Dual SIM LTE (ZP951), ZTE Max+, etc.Д¬hanges in version 8.0.2 (November 19, 2015): Updated live data parsing from Expedia (5.1) from iOS devices.ДЄpplications. Updated live and deleted data parsing from GMail (5.4) from Android devices.ДЄpplications. Updated live and deleted data parsing from ICQ (5.8.1) from iOS devices.ДЄpplications. Updated live and deleted data parsing from Line (5.8.0) from iOS devices.ДЄpplications. Updated live and deleted data parsing from TripIt (5.3.0) from iOS devices.ДЄpplications. Updated live data parsing from Instagram (6.10.1) from iOS devices.ДЄpplications. Updated live and deleted data parsing from Telegram (3.2.2) from iOS devices.ДЄpplications. Updated live and deleted data parsing from Facebook Messenger (50.0) from iOS devices and Facebook Messenger (51.0.0.17.128) from Android devices.ДЄpplications.

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#G OXYGEN FORENSICS MANUAL#

Increased spatial sampling of precipitation, especially for high elevation regions, and temporal sampling of ground and tap water would considerably aid isotopic studies in this > manual > Documentation However, large discrepancies between modelled isotopic composition of precipitation and our ground water and tap water isoscapes, particularly at higher elevations, highlighted uncertainty in the accuracy of modelled precipitation isoscapes for this region. Оґ 2H and Оґ 18O of ground water, and to a lesser extent tap water, reflected the Оґ 2H and Оґ 18O of long-term weighted annual precipitation at the two GNIP stations in South Africa. This spatial structure resulted in considerable differences in isotopic composition of water in many of the major wildlife reserves in South Africa, indicating a good potential for wildlife forensics in this region. We found coherent spatial structure in Оґ 2H, Оґ 18O and d of ground water and tap water that could be predicted by a geostatistical model based on simple environmental parameters (elevation, mean annual precipitation, precipitation minus potential evaporation, distance to coast and modeled isotope ratio of precipitation). Ground water and tap water samples were collected from across South Africa, analysed for Оґ 2H and Оґ 18O, and used to generate interpolated Оґ 2H, Оґ 18O and deuterium-excess ( dВ =В Оґ 2H вЂ“ 8*Оґ 18O) isoscapes.

We compare and contrast these two water resources, and consider how well global models of precipitation isotopes capture isotopic variation across South Africa. Here we present the first ground water and tap water isoscapes for southern Africa. Southern Africa is a globally important meeting point for ocean and climate systems, biological diversity and human societies, yet there is little information on the spatial variability of Оґ 2H and Оґ 18O in water across this important region. Physical processes result in spatial variation of Оґ 2H, Оґ 18O in water across the landscape (so-called вЂњisoscapesвЂќ) and provide the basis for hydrological, ecological, archaeological and forensic studies. Оґ 2H and Оґ 18O of water are incorporated into geological and biological systems in a predictable manner and have been used extensively as tracers in hydrological, ecological and forensic studies. Stable isotopes in water (Оґ 2H and Оґ 18O) are important indicators of hydrological and ecological pattern and process.

G oxygen forensics