scholarly journals Geophysical Measurements to Determine the Hydrologic Partitioning of Snowmelt on a Snow‐Dominated Subalpine Hillslope

2018 ◽  
Vol 54 (6) ◽  
pp. 3788-3808 ◽  
Author(s):  
Drew Thayer ◽  
Andrew D. Parsekian ◽  
Kevin Hyde ◽  
Heather Speckman ◽  
Dan Beverly ◽  
...  
Keyword(s):  
Geophysical Measurements ◽  
Hydrologic Partitioning

Non-Contact Micro-Geophysical Measurements in the Study of Wall Structures.

2008 ◽  
Vol 1 (2) ◽  
pp. 154-176 ◽  
Author(s):  
G. Ranieri ◽  
R. Deiana ◽  
C. Piga
Keyword(s):  
Wall Structures ◽  
Geophysical Measurements

In search of the camp of the IV Scythian legion near ancient Artaxata: research at Pokr Vedi 2015–2018

2020 ◽  
pp. 409-432
Author(s):  
Oskar Kubrak ◽  
Paulina Kubrak ◽  
Mkrtich H. Zardaryan
Keyword(s):  
Electrical Resistivity ◽  
Aerial Photography ◽  
Magnetic Measurements ◽  
Roman Army ◽  
Field Surveys ◽  
Non Invasive ◽  
Southern Border ◽  
Building Activities ◽  
Geophysical Measurements ◽  
Selection Of

During the last years of Emperor Trajan’s reign, the Legio IV Scythica was stationed in the capital of Armenia at that time, Artaxata. It had made its way there within the scope of the Roman campaign against the Parthians. Its presence was immortalised on stamped rooftiles, bricks and a monumental inscription discovered by the southern border of the present-day village of Pokr Vedi. The inscription carved into limestone confirms the building activities of the Roman army. Similar inscriptions were frequently placed on the gates and most important buildings in legionary camps. Polish and Armenian archaeologists undertook a joint search for the supposed camp of the Fourth Scythian Legion in the vicinity of the present-day village of Pokr Vedi, where the above-mentioned construction inscription had been found. The field surveys conducted within the framework of the Pokr Vedi Project were mainly of a non-invasive character. The following were applied: surface prospection, aerial photography, interviews with the inhabitants, scanning of part of the terrain and geophysical measurements done using two methods: electrical resistivity and magnetic measurements. The accumulated data enabled the selection of sites in which survey trenches were located

Integrated Efforts for Analysis of Geophysical Measurements and Models.

1997 ◽  
Author(s):  
S. M. Ayer ◽  
C. A. Hein ◽  
G. P. Seeley ◽  
J. N. Bass ◽  
M. J. Kendra
Keyword(s):  
Geophysical Measurements

scholarly journals Complementary Use of Magnetometric Measurements for Geochemical Investigation of Light REE Concentration in Anthropogenically Polluted Soils

Minerals ◽  
2021 ◽  
Vol 11 (5) ◽  
pp. 457
Author(s):  
Piotr Fabijańczyk ◽  
Jarosław Zawadzki
Keyword(s):  
Soil Samples ◽  
Soil Conditions ◽  
Soil Cores ◽  
Light Rare Earth ◽  
Polluted Soils ◽  
Chemical Measurements ◽  
Geochemical Investigation ◽  
Light Rare Earth Elements ◽  
Soil Magnetic Susceptibility ◽  
Geophysical Measurements

The purpose of this study was to use fast geophysical measurements of soil magnetic susceptibility (κ) as supplementary data for chemical measurements of selected light rare earth elements (REEs) in soil. In order to ensure diversity in soil conditions, anthropogenic conditions and types of land use, seven areas were selected, all located in regions subjected to past or present industrial pollution. Magnetometric parameters were measured using a selected magnetic sensor that was specially designed for measurements of soil cores and were used to classify collected soil cores into six distinctive types. The analysis of REEs concentrations in soil was carried out taking into account the grouping of collected soil samples based on the type of study area (open, forested and mountain), and additionally on the measured magnetometric parameters of collected soil cores. A use of magnetometric measurements provided different, but complementary to chemical measurements information, which allowed to obtain deeper insight on REEs concentrations in soils in studied areas.

Computed Tomography Scanning and Geophysical Measurements of the Wabash No.1 Core

2021 ◽  
Author(s):  
Thomas Paronish ◽  
Rhiannon Schmitt ◽  
Dustin Crandall ◽  
Johnathan Moore ◽  
Carl Carman ◽  
...  
Keyword(s):  
Computed Tomography ◽  
Computed Tomography Scanning ◽  
Tomography Scanning ◽  
Geophysical Measurements

Automatic Plotting of Airborne Geophysical Survey Data

1972 ◽  
Vol 25 (2) ◽  
pp. 162-175 ◽  
Author(s):  
B. M. Ewen Smith
Keyword(s):  
Dead Reckoning ◽  
Geophysical Survey ◽  
The Other ◽  
Ice Thickness ◽  
Terminal Position ◽  
The World ◽  
Geophysical Measurement ◽  
The Antarctic ◽  
Thickness Measurements ◽  
Geophysical Measurements

When geophysical measurements are made from the air, it is important to know the position of the aircraft. The position at any time is usually known from a combination of position-fixing and dead-reckoning systems. In-flight optimization of this combination is a well-studied subject. When post-flight track plotting is required for geophysical survey, use can be made of both the initial and terminal position fixes to correct the dead-reckoning track and hence improve on the in-flight version. This technique is applied to compute the track of aircraft conducting ice thickness measurements in the Antarctic, and the effect of certain errors is evaluated. The algebraic results are equally applicable in parts of the world where better navigational aids are available. A relation is derived between the track plotting errors and die errors in the geophysical measurement such that the precision of one is not degraded by errors in the other.

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