Evolution of the mental picture of shale reservoir completion – 3rd Shale Science Conference (Warsaw, 9–10 June 2014) : note

Journal Title: Geology, Geophysics & Environment - Year 2014, Vol 40, Issue 3

Abstract

Modern measuring equipment is sometimes used for applications, for which it has not been originally designed. For example Ground Penetrating Radar (GPR), designed for subsurface structures analysis, can be used for tree tomography. Radar utilizes the phenomenon of propagation of the electromagnetic waves in a physical medium. Measurements can be carried out in situ, in a non-invasive manner on a living tree. Collected data allow for the tree condition determination. It is possible to detect voids and internal structure. Geophysical investigations can provide an estimation of the risk of falling of the trees. These methods also allow determination of the production quality of the tree by detecting knots inside the structure. Available literature shows only limited examples of the usage of other geophysical surveys, such as the ultrasound and geoelectrical method. However, in many cases these measurements are performed on samples in the form of profiles cut from the felled trees. Presented study was conducted on a set of 8 ash trees growing in the Krakow city parks. The measurement was carried out with high frequency antenna – 1600 MHz. Due to the lack of available literature and limited experience of the authors, only trees with known condition were tested. Despite many attempts, the authors were not able to developed a reliable measurement methodology which would allow for unambiguous classification and interpretation of results. In most cases, the results of the study permitted determination of the trees condition. However, some echograms, of the surveyed trees with visible voids pointed to a different tree state and misclassification. Despite that, the research results seem to be promising and the authors believe in the usefulness of the further development of measurement method along with its extension to other trees species.

Authors and Affiliations

B. Liana, P. Hadro

Keywords

Related Articles

Tools to store information about the environment

Earth Science provide large amounts of data. The available information can be stored and then analysed in different systems. For disciplines such as: geology, geophysics and environmental protection are created database....

Significance of pressure solution structures analysis for fluid flow studies - examples from Struga 1 well (Zechstein Main Dolomite; W Poland) – first results

The internal structure and composition of pressure solution structures are factors that may influence petroleum generation and migration (Hofmann & Leythaeuser 1995). Pressure solution structures (PSS) i.e. stylolites an...

The influence of trade contacts on grave equipment of Gniew community in the 14th-18th century

Richness and variety of grave equipment (silk textiles, scapulars, crosses, rosaries and the other objects), revealed during archaeological exploration carried out in St. Nicolas church in Gniew and in the area of the fo...

New Species of Anaplecta BURMEISTER, 1838 (Blattaria) from Chiapas Amber, Mexico

Order Blattaria (cockroaches) originated in Late Carboniferous (Brongniart 1885, Zhang et al. 2012) and during its evolution adapted to various environments gaining diverse morphological adaptations including diversifica...

Sedimentary petrology characteristics and their implications for provenance of Hoanh Bo Basin Neogene system in Quang Ninh province, north-eastern Vietnam

The Hoanh Bo Basin has developed over multiple periods since the Miocene period in association with the tectonic activity of the Chi Linh-Hon Gai and Trung Luong Faults. The basin is filled with Neogene continental sedim...

Download PDF file
  • EP ID EP165544
  • DOI 10.7494/geol.2014.40.3.291
  • Views 52
  • Downloads 0

How To Cite

B. Liana, P. Hadro (2014). Evolution of the mental picture of shale reservoir completion – 3rd Shale Science Conference (Warsaw, 9–10 June 2014) : note. Geology, Geophysics & Environment, 40(3), 297-299. https://europub.co.uk/articles/-A-165544