Laboratory and field evaluations of the LISST-100 instrument for suspended particle size determinations

被引:115
作者
Gartner, JW [1 ]
Cheng, RT
Wang, PF
Richter, K
机构
[1] US Geol Survey, Div Water Resources, Menlo Park, CA 94025 USA
[2] Space & Naval Warfare Syst Ctr, Marine Environm Qual Branch, San Diego, CA USA
关键词
laser in-situ scattering and transmissometry; particle size distribution; suspended solids concentration; San Francisco Bay; California;
D O I
10.1016/S0025-3227(01)00137-2
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Advances in technology have resulted in a new instrument that is designed for in-situ determination of particle size spectra. Such an instrument that can measure undisturbed particle size distributions is much needed for sediment transport studies. The LISST-100 (Laser In-Situ Scattering and Transmissometry) uses the principle of laser diffraction to obtain the size distribution and volume concentration of suspended material in 32 size classes logarithmically spaced between 1.25 and 250 mum This paper describes a laboratory evaluation of the ability of LISST-100 to determine particle sizes using suspensions of single size, artificial particles. Findings show the instrument is able to determine particle size to within about 10% with increasing error as particle size increases. The instrument determines volume (or mass) concentration using a volume conversion factor C-v. This volume conversion factor is theoretically a constant. In the laboratory evaluation C,is found to vary by a factor of about three over the particle size range between 5 and 200 mum. Results from field studies in South San Francisco Bay show that values of mass concentration of suspended marine sediments estimated by LISST-100 agree favorably with estimates from optical backscatterance sensors if an appropriate value of C-v, according to mean size, is used and the assumed average particle (aggregate) density is carefully chosen. Analyses of size distribution of suspended materials in South San Francisco Bay over multiple tide cycles suggest the likelihood of different sources of sediment because of different size characteristics during flood and ebb cycles. (C) 2001 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:199 / 219
页数:21
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