Temporal-spatial variations of euphotic depth of typical lake regions in Lake Taihu and its ecological environmental significance

By using the data of underwater irradiance measured in the different lake regions of Lake Taihu during 1998-2004 and total suspended solids (TSS), wind speeds of the total 13 stations in typical lake regions during 1993-2003, this paper analyzes the factors of influencing on PAR (pho- tosynthetically available radiation) attenuation, euphotic depth, and presents the temporal and spatial variations of euphotic depth of typical lake regions in Lake Taihu, and the spectral distributions of euphotic depth at station 2. The results show that the concentration of TSS is the most important factor impacting PAR attenuation, followed by chlorophyll a; chromophoric dissolved organic matter (CDOM) has little impact on the PAR euphotic depth. During 1993-2003, the mean yearly PAR eu- photic depths of the typical lake regions ranged from 1.04 to 1.95 m with a mean value of 1.35±0.23 m. The PAR euphotic depth fell into 3 spatial zone types: Type I, the lowest, including the lake center and the inflows of rivers; Type II, intermediate, including Meiliang Bay, Wulihu Lake and Gonghu Bay; Type III, the greatest, including the East Lake Taihu; corresponding mean depths were approximately 1.1, 1.4, 2.0 m, respectively. The seasonal variations of euphotic depths were not quite the same in different lake regions. In the lake center, the mean values of PAR euphotic depth in summer and au- tumn were significantly greater than those in winter and spring; in the Meiliang Bay, winter means were significantly greater than in the other three seasons; in the East Lake Taihu, winter means were significantly less than in the other three seasons. However, no distinct seasonal change was recorded in the Wulihu Lake, Gonghu Bay and the inflows of rivers. The spectral distributions of euphotic depth present a minimal value at the blue light wave band of 400 nm, and a peak at the green light wave band of around 580 nm. In 1998 and 1999, based on the seasonal many-day continuous measure- ments, the PAR euphotic depths at station 2 were recorded 2.00±0.21, 2.52±0.45, 1.58±0.24, 2.00 ±0.15 m in spring, summer, autumn and winter, respectively. The peak value of 440 nm absorbed by phytoplankton corresponded to a euphotic depth of only 0.81-1.47 m (mean 1.07±0.29 m), which was much lower than the mean PAR euphotic depth of 1.98±0.41 m.

[1]  C. Yentsch,et al.  The Estimation of Phytoplankton Production in the Ocean from Chlorophyll and Light Data1 , 1957 .

[2]  M. Schallenberg,et al.  Effects of sediment resuspension on phytoplankton production: teasing apart the influences of light, nutrients and algal entrainment , 2004 .

[3]  Edward J. Phlips,et al.  Chlorophyll a, tripton, color, and light availability in a shallow tropical inner-shelf lagoon, Florida Bay, USA , 1995 .

[4]  Tim A. Wool,et al.  A SEDIMENT RESUSPENSION AND WATER QUALITY MODEL OF LAKE OKEECHOBEE 1 , 1997 .

[5]  P. Falkowski,et al.  Photosynthetic rates derived from satellite‐based chlorophyll concentration , 1997 .

[6]  H. J. D. Lange The attenuation of ultraviolet and visible radiation in Dutch inland waters , 2000, Aquatic Ecology.

[7]  Macrophyte Influences on Sediment Resuspension and Export in a Shallow Impoundment , 1994 .

[8]  Long and short term variations in suspended particulate material: the influence on light available to the phytoplankton community , 2003 .

[9]  X. Bin,et al.  The Significance of the Research on the Environment Evolution from the Lakes of M onsoon R egion in the Historical Period , 1998 .

[10]  Zygmunt Lorenz,et al.  The influence of vertical mixing on the photoinhibition of variable chlorophyll a fluorescence and its inclusion in a model of phytoplankton photosynthesis , 2003 .

[11]  Kohei Mizobata,et al.  Variability of Bering Sea eddies and primary productivity along the shelf edge during 1998-2000 using satellite multisensor remote sensing , 2004 .

[12]  M. Abbott,et al.  Phytoplankton chlorophyll distibutions and primary production in the Southern Ocean , 2000 .

[13]  Hendrik Schubert,et al.  Evaluation of the different levels of variability in the underwater light field of a shallow estuary , 2001, Helgoland Marine Research.

[14]  Boqiang Qin,et al.  Dynamics of sediment resuspension and the conceptual schema of nutrient release in the large shallow Lake Taihu, China , 2004 .

[15]  C. Cerco,et al.  Modeling underwater light climate in relation to sedimentation, resuspension, water quality and autotrophic growth , 2001, Hydrobiologia.

[16]  F. Delgadillo-Hinojosa,et al.  The Effect of Vertical Mixing on Primary Production in a Bay of the Gulf of California , 1997 .

[17]  Xabier Irigoien,et al.  Light Limitation and Distribution of Chlorophyll Pigments in a Highly Turbid Estuary: the Gironde (SW France) , 1997 .

[18]  E. Donk,et al.  Lakes in the Netherlands, their origin, eutrophication and restoration: state-of-the-art review , 2002 .

[19]  B. Leoni,et al.  Studies on the phytoplankton of the deep subalpine Lake Iseo , 2003 .

[20]  R. Sommaruga,et al.  Changes in UV penetration associated with marine intrusions and freshwater discharge in a shallow coastal lagoon of the Southern Atlantic Ocean , 2000 .

[21]  B. Osborne,et al.  Light and Photosynthesis in Aquatic Ecosystems. , 1985 .

[22]  R. D. Doyle,et al.  Impacts of Water Column Turbidity on the Survival and Growth of Vallisneria americana Winterbuds and Seedlings , 2001 .

[23]  J. Barko,et al.  Sediment resuspension and light attenuation in Peoria Lake: can macrophytes improve water quality in this shallow system? , 2004, Hydrobiologia.

[24]  A Review and Prospect about the Aquatic Environment Studies in Taihu Lake , 1998 .

[25]  C. D. Dieter The Importance of Emergent Vegetation in Reducing Sediment Resuspension in Wetlands , 1990 .

[26]  H. Arst,et al.  Optical and biological properties of Lake Ülemiste, a water reservoir of the city of Tallinn II: Light climate in Lake Ülemiste , 2001 .

[27]  Guosheng Li,et al.  Remote sensing model and dynamic mechanism for seasonal changes of the euphotic depth in the East China Sea , 2003 .