Journal of Tropical Oceanography ›› 2018, Vol. 37 ›› Issue (5): 74-85.doi: 10.11978/2018017CSTR: 32234.14.2018017

Special Issue: 南海专题

• Orginal Article • Previous Articles     Next Articles

Characterization of particle size distribution in the South China Sea basin during summer 2016

Wendi ZHENG1,2(), Wen ZHOU1(), Wenxi CAO1, Guifen WANG1,3, Lin DENG1,2, Wenlong XU1,2, Zhantang XU1, Cai LI1, Jiannan CAI4   

  1. 1. State Key Laboratory of Tropical Oceanography (South China Sea Institute of Oceanology, Chinese Academy of Sciences), Guangzhou 510301, China
    2. University of Chinese Academy of Sciences, Beijing 100049, China
    3. College of Oceanography, Hohai University, Nanjing 210098, China
    4. State Key Laboratory of Marine Environmental Science (Xiamen University), Xiamen 361005, China;
  • Received:2018-02-08 Revised:2018-04-09 Online:2018-09-20 Published:2018-10-13
  • Supported by:
    National Natural Science Foundation of China (41576030, 41431176, 4176045, 4176044, 41376042);Open Research Program of the State Key Laboratory of Tropical Oceanography (LTOZZ1602);Science and Technology Program of Guangzhou, China (201504010034, 201707020023, 201607020041);Science and Technology Planning Project of Guangdong Province of China (2016A020222008);Strategic Priority Programme of the Chinese Academy of Sciences (XDA11040302)

Abstract:

Particle size distribution (PSD) describes the relationship between particle concentration and particle size, influencing marine ecosystem environment, the optical properties of sea water, and so on. Based on the in-situ profiles of biological and optical properties during summer 2016 in the South China Sea basin, characterization of PSD was studied. The power-law model was fit to describe the PSD, and the results indicated that the mean coefficient of determination between in-situ PSD and simulated PSD could reach 0.95 in the logarithmic space. The PSD slope (ξ) ranged in [1.27, 7.65] with a mean of 3.93±0.56. The mean of ξ in the surface water of the South China Sea basin was similar to the mean of ξ in global ocean surface water, but higher than that in the surface water of other areas such as the bay. There was a strong negative relationship between ξ and the mean diameter (DA). Taking section T1 as an example, we analyzed the mean PSD profile of these stations. The features of PSD profiles are as follows. 1) At the surface, there were high values of ξ with low values of DA because the dominate particle was pico-phytoplankton. 2) The minimum value of ξ appeared in the subsurface chlorophyll maximum layer (SCML) with higher DA, which may result from the higher proportion of big phytoplankton. 3) In the twilight layer, the values of ξ as well as the values of DA were between those at the surface and in the SCML. This phenomenon may be related to the process of flocculation, decomposition, and settlement of phytoplankton. The traits of PSD would influence the inherent optical properties (IOP) of seawater. We found that both particulate beam scattering coefficient at 532 nm (bp(532)) and particulate beam backscattering coefficient at 532 nm (bbp(532)) would be higher in the SCML because of the increasing chlorophyll-a concentration. However, the lowest mean bp(532) and the lowest mean bbp(532) were found in the twilight layer. Furthermore, although the relationship between ξ and the particulate beam attenuation sepctral slope was weak, the model of Boss et al. (2001b) is suitable for estimating the regional range and mean value of ξ roughly.

Key words: South China Sea basin, particle size distribution (PSD), PSD slope, mean diameter, optical properties

CLC Number: 

  • P733.3