Analytical Approaches to the Description of Optical Microresonator Devices
Summary (2 min read)
Introduction
- A key risk for hydrocarbon exploration in southern Libya is source rock presence.
- This is based on the assumption that U is not able to migrate as a result of weathering processes during rock exposure at the surface, an assumption that has been the subject of some debate (e.g., Chabaux et al. 2003).
- Therefore, a radioactive peak on the gamma-ray log may also be caused by elevated Th and K contents but may be unrelated to U.
Geological setting
- The present study focuses on Jabal Eghei, on the western margin of basin.
- The oldest studied succession, the Hawaz Formation, composed of a cross-bedded and a Skolithos-burrowed sandstone facies association, occupies the westernmost part of the study area, although isolated outcrops have also been found near the eastern margin of the area.
- The complete thickness of the Hawaz Formation is unknown, but may exceed 100 m (Fig. 2).
- Hand-held gamma-ray measurements enable understanding of the Tanezzuft Formation to be refined by dividing it into three members.
Material and methods
- A portable hand-held gamma-ray spectrometer from GF Instruments (formerly Geofyzika, Brno) was used during fieldwork in November‒December 2008 to determine the in situ concentration of radioactive K, U and Th on outcrop exposures.
- The localities where measurements were performed are shown in Figure 1.
- To deduce the mineralogical composition of the Tanezzuft Formation sediments, X-ray diffraction (XRD) analyses were performed on three representative samples.
- The machine operating conditions were set at 35 kV, 40 mA utilising automatic slits and a step size of 0.02º.
- The samples were prepared as randomly oriented powder samples to which an internal standard of 25% by weight of corundum was added.
Results
- In total, 179 in situ measurements of K, U and Th were performed covering outcrop exposures of the Hawaz, Mamuniyat and Tanezzuft Formations and of the Mesozoic sandstone.
- In the following sections, the data are discussed to discriminate (i) between sandstones and mudrock, (ii) between sandstones from different formations, and (iii) between different members of the Tanezzuft Formation.
- Hawaz Formation and Mamuniyat Formation sandstones and the Mesozoic sandstone show a similar range for Th and U contents, with 2 to 10 ppm for Th and 1 to 3.5 ppm for U. Tanezzuft Formation discrimination Hand-held gamma-ray measurements of the Tanezzuft Formation indicate differences in K content between the three members (Fig. 8).
- The majority of the samples from the lower member have Th/K values >28, those from the middle member range from 3.5‒12, whilst samples from the upper member have Th/K values between 12 and 28 (Fig. 8E).
Discussion
- Origins of the gamma-ray signal Before interpreting the observed K, U and Th values, it is useful to discuss the primary factors controlling the K, U and Th signals and the secondary parameters which modify these values during weathering and diagenesis.
- The commonly observed close relationship between U and TOC contents (Stocks and Lawrence 1990; Lüning and Kolonic 2003) is based on the fact that in seawater U6+ is carried in solution as uranyl carbonate complexes which 'precipitate' under oxygen-depleted, strongly reducing conditions within the sediment during deposition (Wignall and Myers 1988; Klinkhammer and Palmer 1991).
- Ratios of Th/K enable identification of the dominant mineral type (Fig. 8F), with increasing Th/K values from glauconite → muscovite → illite → mixed-layer clays (illite–smectite) → kaolinite → chlorite → bauxite (Bateman 1985).
- The upper member of the Tanezzuft Formation (Figs. 3 and 9), containing the graptolite-bearing bed and kaolinite-rich succession, was likely deposited during greenhouse conditions (warm and at least seasonally humid climate) (Fig. 10).
Conclusions
- Hand-held gamma-ray measurements in outcrop at Jabal Eghei reveal distinct K, U and Th contents for sandstones and mudrocks, which reflect the different mineralogical composition of these strata.
- Mudrocks show higher values of K, U and Th because they are enriched in clay minerals.
- Kaolinite presence probably suggests a relatively humid and warm climate during deposition, if recycling of kaolinite from older successions is excluded.
- The present study clearly shows the applicability of hand-held gamma-ray measurements for chemostratigraphy even in heavily weathered sections in the Libyan Sahara.
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Frequently Asked Questions (11)
Q2. What is the effect of the tuning mechanism on the cavity?
Disregarding its influence on the performance of the (short) couplers as a first approximation, a tuning mechanism, modeled by a small parameter p, affects mainly the light propagation along the cavity ring.
Q3. What is the effect of the two facets at the ends of the cavity?
The two facets at the ends of the cavity segment cause strong reflections of the waves that are excited inside the cavity, while one can assume that they have much less influence on the waves that travel along the port cores.
Q4. What is the effect of the coupler on the power transfer between the straight and the bend core?
As expected, in general the net power transfer between the straight and the bend core grows with decreasing gap width, i.e. with increasing interaction strength, and with increasing bend radius, i.e. with increasing interaction length.
Q5. What is the approximate constraint of lossless couplers?
(3)(The approximate constraint of lossless couplers requires |ρ|2 + |κ|2 = 1 and |κ|2 + |τ|2 = 1, consequently |ρ|2 = |τ|2 = 1 − |κ|2. Provided the input- and output planes are placed properly, one can even restrict to ρ = τ .
Q6. What is the characterization of a dielectric rectangle?
According to the former quantitative characterization in terms of amplification factors based on eigenvalues of Ω, high quality resonances in a dielectric rectangle require a facet reflectivity close to unity for the contributing cavity modes.
Q7. What is the definition of a bimodal resonance?
While this refers to a single mode resonance with a field based upon only one (forward and backward propagating) mode per axis, a bimodal resonance is characterized by the existence of a pair of modes per axis orientation that satisfy the phase relations simultaneously.
Q8. What is the symmetry of the coupler?
Due to the additional symmetry of the coupler element with respect to the vertical plane z = 0 one can expect the transmission A+ → b+ to be equal to the transmission B− → a−.
Q9. What is the effect of the couplers on the ring?
If additionally the radius of the bent core is increased (bottom), one arrives at a configuration with a coupling coefficient |κ|2 that is almost equal to the one of the structure at the top, i.e. the couplers effect similar levels of power transfer between the straight and the bend waveguide, despite the fact that the strength as well as the length of the interaction is much larger in the bottom configuration with larger bend radius andsmaller gap width.
Q10. What is the proper way to compute the resonator spectrum?
Hence the proper way to compute the resonator spectrum would be to evaluate the properties of the port waveguides, the cavity segments, and of the coupler regions as input for the above expressions, for a series of wavelengths.
Q11. What is the approximation of L = 2R?
R (though one frequently encounters the approximation L = 2πR corresponding to an interaction length that is short when compared to the cavity ring).