Duan H, Ma R, Loiselle SA et al. Optical characterization of black water blooms in eutrophic waters. Science of the Total Environment, 2014, 482:174-183.
Shen Q, Zhou Q, Shang J et al. Beyond hypoxia: Occurrence and characteristics of black blooms due to the decomposition of the submerged plant Potamogeton crispus in a shallow lake. Journal of Environmental Sciences, 2014, 26(2): 281-288.
[7]
Liu C, Shen Q, Zhou Q et al. Precontrol of algae-induced black blooms through sediment dredging at appropriate depth in a typical eutrophic shallow lake. Ecological Engineering, 2015, 77: 139-145.
He YT, Wilson JT, Wilkin RT. Transformation of reactive ironminerals in a permeable reactive barrier (biowall) used to treat tce in groundwater. Environmental Science and Technology, 2008, 42(17):6690-6696.
[10]
Luther Lii GW, Glazer B, Ma S et al. Iron and sulfur chemistry in a stratified lake:evidence for iron-rich sulfide complexes. Aquatic Geochemistry, 2003, 9:87-110.
Shen Q, Liu C, Zhou Q et al. Effects of physical and chemical characteristics of surface sediments in the formation of shallow lake algae-induced black bloom. Journal of Environmental Sciences, 2013, 25(12): 2353-2360.
[15]
Rozan TF, Taillefert M, Trouwborst RE et al. Iron-sulphur-phosphorus cycling in the sediments of a shallow coastal bay:Implications for sediment nutrient release and benthic macroalgal blooms. Limnology and Oceanography, 2002, 47(5):1346-1354.
[16]
Hsieh YP, Shieh YN. Analysis of reduced inorganic sulfur by diffusion methods:improved apparatus and evaluation for sulfur isotopic studies. Chemical Geology, 1997, 137(3/4):255-261.
[17]
Feng Z, Fan C, Huang W et al. Microorganisms and typical organic matter responsible for lacustrine “black bloom”. Science of the Total Environment, 2014, 470:1-8.
