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Single measurements were taken from each sample on the upper and lower surfaces according to the in situ orientation at time of sampling (measurements on upper surface only for static control corals), following methodology described in Burdett et al.24 with an Ocean Optics USB 2000+ spectrometer.
Excised axially oriented lingual core tissues (fresh or paraffin-embedded) were also imaged with a mode-locked Ti-Sapphire laser, (76 MHz repetition rate, 150 femtosecond pulse width), allowing for the visualization of individual myofibers at in situ orientation.
In situ orientation was determined by anatomical landmarks.
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In this paper, we review a suite of techniques for determination of in situ stress orientation and magnitude in deep wells and boreholes.
Targets and problems of the future Japanese project ILOM (In situ Lunar Orientation Measurement), which is planned to be realized as one kind of observations of lunar rotation at the second stage of SELENE-2 mission, are briefly described in the article.
Borehole breakouts are enlargements and elongation of a borehole in a particular direction, caused by failure of the borehole wall rock due to concentration of stresses around the borehole, and thus, have been widely used to determine the in situ stress orientation.
This eliminates the requirement of in-situ stress orientation for designing multi-hydraulic water-fracturing horizontal wells.
We investigated the in-situ molecular orientation behavior of isotactic polypropylene (iPP) films under simultaneous and sequential biaxial deformation by polarized infrared spectroscopy at near melting temperature.
Measurements of in-situ stress orientations at relatively shallow depths were conducted at 11 sites along the Anninghe-Zemuhe fault zone, southwestern China, with a newly developed method.
The analysis results substantiate the previous understanding that the success of the hydraulic fracturing process not only depends on controllable parameters such as fracture fluid properties and injection rate, but also relies on the uncontrollable parameters such as ground in-situ stress regime, orientation of principal stresses, and in-situ rock mass properties.
The cores were oriented in-situ using an orientation device equipped with both a magnetic compass and a sun compass.
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