An improved method of laser particle size analysis and its applications in identification of lacustrine tempestite and beach bar: An example from the Dongying depression

Yuanfu Zhang , Chenlin Hu , Xingmou Wang , Min Wang , Zaixing Jiang , Junjie Li

Journal of Earth Science ›› 2017, Vol. 28 ›› Issue (6) : 1145 -1152.

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Journal of Earth Science ›› 2017, Vol. 28 ›› Issue (6) : 1145 -1152. DOI: 10.1007/s12583-016-0930-1
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An improved method of laser particle size analysis and its applications in identification of lacustrine tempestite and beach bar: An example from the Dongying depression

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Abstract

Grain size analysis is a common method in the study of sedimentology. For the consolidated sedimentary rocks, the traditional methods are rock slice observation and image analysis. In recent years, laser particle size analyzer is used widely in particle size analysis of sedimentary rock. Unlike the pretreatment of loose samples, the rock samples must be crushed, added acid to wipe out cement, and washed. However, in the step of washing, most of the fines component (less than 63 μm) in the suspended state should be inevitably lost. It will significantly affect the accuracy of particle size analysis, especially for siltstone. This paper presents a siltstone sample pretreatment method which core step is washing acid by centrifuge. Compared with traditional decantation method, the results show that the median particle size reduced 33.2 μm on average. Compared with the precipitation method which is commonly used for handling loose samples, the change of solid-liquid separation time is from 12 h to 10 min, while the average reduction of median particle size is about 15 μm. The grain size value corresponded to the cumulative volume of 10%/90% reduced 2.5 μm/20.3 μm on average. The percentage of the clay component less than 2 μm increased 2.88% on average. The fine particle (2–4 μm) and silt component (4–63 μm) increased 1.71% and 5.56% on average. Based on this method, two kinds of similar lacustrine siltstone were analyzed. They are tempestite and beach bar which are difficult to identify in the Lijin sub-depression, Dongying depression, Shengli oilfield, China. The final grain-size probability plot of tempestite is the type of “one saltation component and three suspension components”. The content of suspension components can reach to 80%–90%. The beach bar is the type of “one saltation component and two suspension components”. The content of suspension components can reach to 40%–45%. They both have the characteristics of high slope which means well sorting. But they can be distinguished based on the suspension sedimentary characteristics which were preserved by maximum degree in this kind of sample pretreatment method.

Keywords

siltstone / grain size analysis / sample pretreatment / washing acid / centrifuge

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Yuanfu Zhang, Chenlin Hu, Xingmou Wang, Min Wang, Zaixing Jiang, Junjie Li. An improved method of laser particle size analysis and its applications in identification of lacustrine tempestite and beach bar: An example from the Dongying depression. Journal of Earth Science, 2017, 28(6): 1145-1152 DOI:10.1007/s12583-016-0930-1

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References

[1]

Allen T. Particle Size Measurement, 1984, 219-414.

[2]

Beuselinck L., Govers G., Poesen J., . Grain-Size Analysis by Laser Diffractometry: Comparison with the Sieve-Pipette Method. Catena, 1998, 32(3/4): 193-208.

[3]

Bianchi G. G., Hall I. R., McCave I. N., . Measurement of the Sortable Silt Current Speed Proxy Using the Sedigraph 5 100 and Coulter Multisizer IIe: Precision and Accuracy. Sedimentology, 1999, 46(6): 1001-1014.

[4]

Blott S. J., Pye K. Particle Size Distribution Analysis of Sand-Sized Particles by Laser Diffraction: An Experimental Investigation of Instrument Sensitivity and the Effects of Particle Shape. Sedimentology, 2006, 53(3): 671-685.

[5]

Cao Y. C., Wang J., Liu H. M., . Sedimentary Characteristics and Models of Beach-Bar Sandbodies in the Upper Part of the Fourth Member of Paleogene in the South Slope of Dongying Depression. Journal of China University of Petroleum, 2009, 33(6): 5-10.

[6]

Cheetham M. D., Keene A. F., Bush R. T., . A Comparison of Grain-Size Analysis Methods for Sand-Dominated Fluvial Sediments. Sedimentology, 2008, 55(6): 1905-1913.

[7]

Cheng P., Gao S., Li X. S. Evaluation of a Wide Range Laser Particle Size Analysis and Comparison with Pipette and Sieving Methods. Acta Sedimentologica Sinica, 2001, 19(3): 449-454.

[8]

Ding X. G., Ye S. Y., Gao Z. J. Development and Application of Grain Size Analysis Technique. Global Geology, 2005, 24(2): 203-207.

[9]

Goossens D. Techniques to Measure Grain-Size Distributions of Loamy Sediments: A Comparative Study of Ten Instruments for Wet Analysis. Sedimentology, 2007, 55(1): 65-96.

[10]

Hu C. L., Zhang Y. F., Jiang Z. X., . Morphologic Changes in Modern Onshore Beach Bar of Poyang Lake under Wind and Wave Actions. Acta Petrolei Sinica, 2015, 36(12): 1543-1552.

[11]

Jiang Z. X. Sedimentology, 2010, 159-161.

[12]

Jiang Z. X., Liu L. A. A Pretreatment Method for Grain Size Analysis of Red Mudstones. Sedimentary Geology, 2011, 241(1/2/3/4): 13-21.

[13]

Konert M., Vandenberghe J. Comparison of Laser Grain Size Analysis with Pipette and Sieve Analysis: A Solution for the Underestimation of the Clay Fraction. Sedimentology, 1997, 44(3): 523-535.

[14]

Liu S. C. The Characteristics of Tempestite and the Different Sign Contrasting with Turbidites. Sedimentary Facies and Palaeogeography, 1989, 5: 44-55.

[15]

Ma Y. S., Zhong L. Recent Development of Study on Storm Deposition and Tempestites. Geological Science and Technology Information, 1990, 9(3): 9-14.

[16]

Pang J. L., Qiao J., Huang C. C. Pretreatment Methods and Their Influences on Grain-Size Measurement of Palaeosol in the Upper Reaches of the Hanjiang River Valley, China. Scientia Geographica Sinica, 2013, 33(6): 748-754.

[17]

Technical Committee on Standardization of Petroleum Geological Exploration, 2010. Analysis Method for Particle Size of Clastic Rocks, SY/T 5434–2009. Petroleum Industry Press, Beijing. 1–17

[18]

Rubin D. M., Chezar H., Harney J. N., . Underwater Microscope for Measuring Spatial and Temporal Changes in Bed-Sediment Grain Size. Sedimentary Geology, 2007, 202(3): 402-408.

[19]

Singer J. K., Anderson J. B., Ledbetter M. T., . An Assessment of Analytical Techniques for the Size Analysis of Fine-Grained Sediments. SEPM Journal of Sedimentary Research, 1988, 58(3): 534-543.

[20]

Wang D. J., Fan D. D., Li C. X. Influence of Different Pretreatment on Size Analysis and Its Implication. Journal of Tongji University, 2003, 31(3): 314-318.

[21]

Wang J. B., Zhu L. P. Influence of Different Pre-Treatments on Grain-Size Measurement of Lake Sediments. Journal of Lake Sciences, 2005, 17(1): 17-23.

[22]

Wang J. B., Ju Y. T., Zhu L. P. Comparison of Lake Sediment Grain Size Results Measured by Two Laser Diffraction Particle Size Analyzers. Journal of Lake Sciences, 2007, 19(5): 509-515.

[23]

Wang S. L., Jiang Z. X., Liu H. Sendimentary Characteristics and Model of Tempestites-Beach Bar of Upper Section of the Fourth Member of Shahejie Formation in Boxing Sag. Fault-Block Oil & Gas Filed, 2009, 16(4): 37-39.

[24]

Wang X. G., Zhao B. H. Measurement Technique and Application of Power Particle Size. China Molybdenum Industry, 2002, 26(6): 32-34.

[25]

Wang Y. M., Wang X. H., Gao Y. S. Modern Methods for the Measurement and Characterization of Particle Size in Geostandards Reference Materials. Geological Bulletin of China, 2009, 28(1): 137-145.

[26]

Yuan J., Du Y. M., Li Y. N. Probability Cumulative Grain Size Curves Interrigenous Depositional Environments of the Paleogene in Huimin Sag. Petroleum Exploration and Development, 2003, 30(3): 103-106.

[27]

Yuan W. F., Chen S. Y., Zeng C. M. Probability Cumulative Grain Size Curves in Terrigenous of the Tertiary in West Qaidam Basin. Journal of the University of Petroleum, 2005, 29(5): 12-18.

[28]

Zhang Y. F., Jiang Z. X., Wang Y., . Comparative Analysis of Sequence Characteristics among Different Superimposed Stages of the Chelif Basin, Algeria. Acta Geologica Sinica—English Edition, 2009, 83(6): 1041-1051.

[29]

Zhang Y. F., Jiang Z. X. Outcrop Characterization of an Early Miocene Slope Fan System, Chelif Basin, Algeria. Energy, Exploration & Exploitation, 2011, 29(5): 633-646.

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