The grain size distribution function of suspended load in the lower Yellow River

Zipu Ma

River ›› 2025, Vol. 4 ›› Issue (4) : 470 -487.

PDF
River ›› 2025, Vol. 4 ›› Issue (4) :470 -487. DOI: 10.1002/rvr2.70030
RESEARCH ARTICLE
The grain size distribution function of suspended load in the lower Yellow River
Author information +
History +
PDF

Abstract

The log-normal distribution function (LNDF) and Weibull cumulative density function (WCDF) represent two prevalent approaches for characterizing sediment grain size distributions. This study analyzes annual average suspended load grain size data (standardized to equivalent settling diameters) from seven hydrological stations in the lower Yellow River (LYR) spanning 1962-2020, employing various distribution functions for grain size fitting. Results demonstrate that the Weibull probability density function (WPDF) offers significant advantages over both LNDF and WCDF in terms of fitting accuracy, parameter stability, simplicity, and practical applicability for characterizing suspended load grain size distributions in the LYR. Based on these findings, universal formulas were developed for the suspended load grain size distribution across the seven stations and the entire lower reaches, yielding determination coefficients (R2) exceeding 0.9. These formulas can be applied to estimate suspended load grain size in data-scarce cross-sections. The existence of such universal formulas suggests that interannual fluctuations in suspended load grain size in the LYR are constrained within a limited range, suggesting that sediment grain size may represent an inherent property of the river channel. This limited variability may be attributed to the fact that sediments in the LYR are primarily derived from a relatively fixed source region—the Loess Plateau. The observed stability over an extended period also offers valuable insights into the fundamental properties of river systems and their long-term behavior.

Keywords

grain size / lognormal distribution / suspended load / the lower Yellow River (LYR) / Weibull cumulative density function (WCDF) / Weibull probability density function (WPDF)

Cite this article

Download citation ▾
Zipu Ma. The grain size distribution function of suspended load in the lower Yellow River. River, 2025, 4(4): 470-487 DOI:10.1002/rvr2.70030

登录浏览全文

4963

注册一个新账户 忘记密码

References

[1]

Barndorff Nielsen, O. (1977). Exponentially decreasing distribution for the logarithm of particle size. Proceedings of the Royal Society A, Mathematical, 353, 401-419. https://doi.org/10.1098/rspa.1977.0041

[2]

Blench, T. (1952). Normal size distributions found in samples of river bed sand. Civil Engineering (USA), 22, 147.

[3]

Chien, N. (1959). Change of bed material composition in a degraded bed and its effect on the stabilization of stream channel. Journal of Sediment Research, 1, 16-23. https://doi.org/10.16239/j.cnki.0468-155x.1959.01.002in Chinese.

[4]

Christiansen, C., Blæsild, P., & Dalsgaard, K. (1984). Re-interpreting “segmented” grain size curves. Geological Magazine, 121(1), 47-51. https://doi.org/10.1017/S001675680002793X

[5]

Fang, C., Guan, J., & Shi, H. (2023). Relationship between sediment transport capacity of the Poyang Lake channel and sediment out of the lake and adjustment. Journal of Hydraulic Engineering, 54(8), 997-1004. https://doi.org/10.13243/j.cnki.slxb.20220565 in Chinese

[6]

Fieller, N. R. J., Gilbertson, D. D., Griffin, C. M., Briggs, D. J., & Jenkinson, R. D. S. (1992). The statistical modelling of the grain size distributions of cave sediments using log skew laplace distributions: Creswell Crags, near Sheffield, England. Journal of Archaeological Science, 19(2), 129-150. https://doi.org/10.1016/0305-4403(92)90045-5

[7]

Flenley, E. C., Fieller, N. R. J., & Gilbertson, D. D. (1987). The statistical analysis of ‘mixed’ grain size distributions from aeolian sands in the Libyan Pre-Desert using log skew Laplace models. Geological Society, London, Special Publications, 35(1), 271-280. https://doi.org/10.1144/gsl.sp.1987.035.01.18

[8]

Gan, S. Q., & Scholz, C. A. (2017). Skew normal distribution deconvolution of grain-size distribution and its application to 530 samples from Lake Bosumtwi, Ghana. Journal of Sedimentary Research, 87(11), 1214-1225. https://doi.org/10.2110/jsr.2017.68

[9]

Ghosh, J. K., & Mazumder, B. S. (1981). Size distribution of suspended particles-unimodality, symmetry, and log-normality. In C. Taillie et al. (Eds.), Statistical Distribution in Scientific Work. D. Reidel Publishing Company.

[10]

Ghoshal, K., Purkait, B., & Mazumder, B. S. (2011). Size distributions In suspension over sand-pebble mixture: An experimental approach. Sedimentary Geology, 241(1-4), 3-12. https://doi.org/10.1016/j.sedgeo.2011.09.003

[11]

Hartmann, D. (2007). From reality to model: Operationalism and the value chain of particle-size analysis of natural sediments. Sedimentology, 202(3), 383-401. https://doi.org/10.1016/j.sedgeo.2007.03.013

[12]

Hou, C., Yi, Y., Song, J., & Zhou, Y. (2021). Effect of water-sediment regulation operation on sediment grain size and nutrient content in the lower Yellow River. Journal of Cleaner Production, 279, 123533. https://doi.org/10.1016/j.jclepro.2020.123533

[13]

Hu, C., Chen, J., & Guo, Q. (2012). Shaping and maintaining a medium-sized main channel in the Lower Yellow River. International Journal of Sediment Research, 27(3), 259-270. https://doi.org/10.1016/S1001-6279(12)60034-1

[14]

Hu, C., Zhang, Z., & Zhang, X. (2023). Threshold system of regulation indicators for maintaining the runoff and sediment balance of the Yellow River basin. Advances in Water Science, 34(5), 647-659. https://doi.org/10.14042/j.cnki.32.1309.2023.05.001 in Chinese

[15]

Hwang, S. I., Lee, K. P., Lee, D. S., & Powers, S. E. (2002). Models for estimating soil particle-size distributions. Soil Science Society of America Journal, 66(4), 1143-1150. https://doi.org/10.2136/sssaj2002.1143

[16]

Kittleman, L. R. (1964). Application of Rosin's distribution in size-frequency analysis of clastic rocks. Journal of Sedimentary Research, 34(3), 483-502. https://doi.org/10.1306/74D710C8-2B21-11D7-8648000102C1865D

[17]

Li, P., Zhang, K., Wang, J., & Feng, D. (2021). Response of interrill erosion to flow parameters of sand loess in regions with high and coarse sediment yields. Journal of Hydrology, 592, 125786. https://doi.org/10.1016/j.jhydrol.2020.125786

[18]

Li, W., Zhu, L., Xie, G., Hu, P., & de Vriend, H. J. (2022). Quantification of the influencing factors for flood peak discharge increase in the Lower Yellow River. Journal of Hydrology, 613, 128329. https://doi.org/10.1016/j.jhydrol.2022.128329

[19]

Liu, X., Feng, X., Liu, J., & Lin, L. (2014). Laboratory application of laser grain-size analyzer in determining suspended sediment concentration. Journal of Ocean University of China, 13(3), 375-380. https://doi.org/10.1007/s11802-014-1973-2

[20]

Ma, H., Nittrouer, J. A., Fu, X., Parker, G., Zhang, Y., Wang, Y., Wang, Y., Lamb, M. P., Cisneros, J., Best, J., Parsons, D. R., & Wu, B. (2022). Amplification of downstream flood stage due to damming of fine-grained rivers. Nature Communications, 13(1), 3054. https://doi.org/10.1038/s41467-022-30730-9

[21]

Ma, H., Nittrouer, J. A., Naito, K., Fu, X., Zhang, Y., Moodie, A. J., Wang, Y., Wu, B., & Parker, G. (2017). The exceptional sediment load of fine-grained dispersal systems: Example of the Yellow River, China. Science Advances, 3(5), e1603114. https://doi.org/10.1126/sciadv.1603114

[22]

Ma, Z., Guo, Q., Guan, J., et al. (2022). Vertical distribution of grain size gradation for the non-equilibrium sediment transport conditions. Journal of Sediment Research, 47(4), 1-7. https://doi.org/10.16239/j.cnki.0468-155x.2022.04.001 in Chinese

[23]

Peng, J., Wang, X., Yin, G., Adamiec, G., Du, J., Zhao, H., Kang, S., Hu, G., & Zheng, Y. (2022). Accumulation of aeolian sediments around the Tengger Desert during the late Quaternary and its implications on interpreting chronostratigraphic records from drylands in north China. Quaternary Science Reviews, 275, 107288. https://doi.org/10.1016/j.quascirev.2021.107288

[24]

Qian, N., & Wan, Z. H. (1983). Mechanics of sediment transport. Science Press.in Chinese

[25]

Sengupta, S., Ghosh, J. K., & Mazumder, B. S. (1991). Experimental-theoretical approach to interpretation of grain size frequency distributions. In J. P. M. Syvitski (Ed.), Principles, methods and applications of particle size analyses. Cambridge University Press.

[26]

Shen, G., Zhang, Y., & Shang, H. (2008). Response mechanism of the lower Yellow River to flood and sediment transport law. Yellow River Water Conservancy Pressin Chinese.

[27]

Shih, S. M., & Komar, P. D. (1990). Differential bedload transport rates in a gravel-bed stream: A grain-size distribution approach. Earth Surface Processes and Landforms, 15(6), 539-552. https://doi.org/10.1002/esp.3290150606

[28]

Shirazi, M. A., & Boersma, L. (1984). A unifying quantitative analysis of soil texture. Soil Science Society of America Journal, 48(1), 142-147. https://doi.org/10.2136/sssaj1984.03615995004800010026x

[29]

Sun, D., Bloemendal, J., Rea, D. K., Vandenberghe, J., Jiang, F., An, Z., & Su, R. (2002). Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components. Sedimentary Geology, 152(3-4), 263-277. https://doi.org/10.1016/S0037-0738(02)00082-9

[30]

Sun, L., Zhou, X., Wang, Y., Cheng, W., & Jia, N. (2012). Identification of Paleo-events recorded in the Yellow Sea sediments by sorting coefficient of grain size. PLoS One, 7(9), e44725. https://doi.org/10.1371/journal.pone.0044725

[31]

Wang, S., Fu, B., Piao, S., Lü, Y., Ciais, P., Feng, X., & Wang, Y. (2016). Reduced sediment transport in the Yellow River due to anthropogenic changes. Nature Geoscience, 9(1), 38-41. https://doi.org/10.1038/NGEO2602

[32]

W. C. Krumbein, K. (1938). Size frequency distributions of sediments and the normal phi curve. SEPM Journal of Sedimentary Research, 8, 84-90. https://doi.org/10.1306/d4269008-2b26-11d7-8648000102c1865d

[33]

Wu, B., Wang, G., Xia, J., Fu, X., & Zhang, Y. (2008). Response of bankfull discharge to discharge and sediment load in the Lower Yellow River. Geomorphology, 100(3-4), 366-376. https://doi.org/10.1016/j.geomorph.2008.01.007

[34]

Xia, J., Jiang, Q., Deng, S., Zhou, M., Cheng, Y., Li, Z., & Wang, Z. (2022). Morphological characteristics and evolution processes of sharp bends in the Lower Yellow River. Catena, 210, 105936. https://doi.org/10.1016/j.catena.2021.105936

[35]

Xiao, J., Chang, Z., Si, B., Qin, X., Itoh, S., & Lomtatidze, Z. (2009). Partitioning of the grain-size components of Dali Lake core sediments: Evidence for lake-level changes during the Holocene. Journal of Paleolimnology, 42(2), 249-260. https://doi.org/10.1007/s10933-008-9274-7

[36]

Xiong, Z. (1991). Study on river sediment grain size. River Sediment Research Office, Wuhan Institute of Water Resources and Electric Power. in Chinese

[37]

Xu, J., Hu, C., & Chen, J. (2009). Effect of suspended sediment grain size on channel sedimentation in the lower Yellow River and some implications. Science in China Series E: Technological Sciences, 39(2), 310-317. https://doi.org/10.1007/s11431-008-0269-4

[38]

Xue, B., Zhang, X., Xu, L., et al. (2020). Response law of sediment diameter change in the lower Yellow River to water and sediment regulation in Xiaolangdi reservoir. Journal of North China University of Water Resources and Electric Power (Natural Science Edition, 41(2), 55-62. https://doi.org/10.19760/j.ncwu.zk.2020023

[39]

Yuan, R., Zhang, C., Wang, X., & Zhu, R. (2018). Utilizing skew normal distribution to unmix grain-size distribution of swampy lakeshore: Example from Lake Ulungur, China. Arabian Journal of Geosciences, 11(22), 695. https://doi.org/10.1007/s12517-018-4038-9

[40]

Zeng, M., Fan, D., Sun, X., Wang, S., & Yang, Z. (2011). The grain-size distribution of the suspended particulate matter in the Huanghe Estuary and its adjacent sea area in winter. Acta Oceanologica Sinica, 30(2), 75-83. https://doi.org/10.1007/s13131-011-0107-6

[41]

Zhang, J., Li, Y., Yang, T., Liu, J., Guo, X., & Yao, Y. (2023). A universal grain-size distribution of soil with scaling invariance. European Journal of Soil Science, 74(2), e13354. https://doi.org/10.1111/ejss.13354

[42]

Zhang, R. (1989). River sediment dynamics. Water Resources and Electric Power Pressin Chinese.

[43]

Zhang, Y., Wang, P., Shen, G., et al. (2023). Impact of Xiaolangdi Reservoir operations on flow resistance in the Lower Yellow River. Advances in Water Sciences, 34(6), 858-866. https://doi.org/10.14042/j.cnki.32.1309.2023.06.004 in Chinese

[44]

Zhou, G. (2006). Probability theory and mathematical statistics. Higher Education Press in Chinese.

RIGHTS & PERMISSIONS

2025 The Author(s). River published by Wiley-VCH GmbH on behalf of China Institute of Water Resources and Hydropower Research (IWHR).

PDF

8

Accesses

0

Citation

Detail

Sections
Recommended

/