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Using special disc-shaped samples field dependencies of magnetostriction in parallel and perpendicular directions of the applied magnetic field were obtained by direct measurement.
The numerical model was verified using the results of TDD tests performed on QS samples, field measurements of some documented projects, and the closed-form solutions to circular tunnels in swelling rock.
For the investigation of surface morphology and steady-state optical properties of the as-grown CSNW samples, field emission scanning electron microscopy (FE-SEM) and PL spectroscopy analyses were performed, respectively.
These results remain robust across the two studies even though they used different designs (cross-sectional versus longitudinal), different samples (field versus students) across different countries (United States versus India), and a host of control variables at both the leader and follower levels.
The data collection included approximately 8 h of video-recorded participant observations over a period of one month, digital photographs, student and teacher work samples, field notes, interviews with the teacher before and after each class, group interviews with the students, and video stimulated recall interviews with selected students.
Table 2 Vitrinite reflectance measurement results of studied samples Field name Formation Depth Romin Romax Romean Comment Azadegan Gadvan 3940 0.28 1.29 0.6 Core Azadegan Gadvan 4129 0.37 1.35 0.7 Cutting Azadegan Gadvan 3757 0.56 1.11 0.89 Cutting Azadegan Gadvan 3940 0.28 1.29 0.6 Cutting Azadegan Gadvan 4128 0.37 1.35 0.7 Cutting Mahshahr Gadvan 4400 0.61 0.61 ?
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To characterize the structural property and functional group of the prepared samples, field-emission scanning electron microscopy (FE-SEM), X-ray diffraction (XRD), transmission electron microscopy (TEM), and Fourier transform infrared spectroscopy (FT-IR) analyses were employed.
The effectiveness of this hybrid method wanes when one samples fields whose energy spectrum decays more rapidly near the origin.
Except one sampling field all the sampling fields contain very low phosphorus.
In some other cases however sample field surveys would be needed.
In Section 4, we describe the sample field model for simulation.
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