Transient storage characteristics of an agricultural headwater stream predominated by Phragmites australis
LI Ru-zhong1, WAN Ling-zhi1, CAO Jing-cheng1, ZHANG Rui-gang2, CHEN Guang-zhou3
1. School of Resources and Environmental Engineering, Hefei University of Technology, Hefei 230009, China;
2. School of Civil Engineering, Hefei University of Technology, Hefei 230009, China;
3. School of Environment and Energy Engineering, Anhui Jianzhu University, Hefei 230022, China
From September 2014 to June 2015, eight field tracer experiments were conducted in a 90-m-length stream reach of an agricultural headwater stream, which is dominant of reeds and belongs to the Ershibu River watershed in Hefei city, using a constant-rate injection of NaCl. Based on the data sets of tracer experiments, the relative deviation of the peak values (HI) of the chloride ion concentrations was calculated with the OTIS model at the condition of ignoring the impact of transient storage or not, and the efficiency for transient storage was interpreted by using multiple transient storage metrics. The results showed that all the values of transient storage exchange coefficient (α) were in the order of magnitude of 10-4 in different seasons. The values of HI ranged from 2.60% to 12.54% without considering the interaction between the main channel and transient storage zone, with the mean value of 5.35%. There was a significant logarithm function relationship between HI and discharge (Q), which was decreased gradually with the increase of the value of Q. Moreover, HI had obvious linear relationship with the ratio of cross-sectional area of storage zones to main channel cross-sectional area (As/A), and which was gradually increased with the increase of the As/A. Significant differences were exhibited between the main channel residence time (Tc) and the transient storage residence time (Ts) in all eight tracer experiments, and the transient storage capacity in the spring and early summer was stronger than that in the autumn and winter. The values of As/A and Fmed200 were respectively in the range of 1.036 to 1.627 and 8.10% to 23.03%. This suggested that the stream with a dominant plant of reeds has a higher capacity for transient storage.
Bukaveckas P A. Effects of channel restoration on water velocity, transient storage, and nutrient uptake in a channelized stream[J]. Environ. Sci. Technol., 2007,41(5):1570-1576.
[4]
Stephen M P, Robert A J, Emily H S. Nutrient retention and the problem of hydrologic disconnection in streams and wetlands[J]. Ecosystems, 2012,15(3):435-449.
[5]
Weigelhofer G, Fuchsberger J, Teufl B, et al. Effects of riparian forest buffers on in-stream nutrient retention in agricultural catchments[J]. J. Environ. Qual., 2012,41(2):373-379.
[6]
Adam S W, Robert A P, Michael N G, et al. Variations in surface water-ground water interactions along a headwater mountain stream:Comparisons between transient storage and water balance analyses[J]. Water Resources Research, 2013,49(6):3359-3374.
[7]
Robert O H Jr, Bernhardt E S, Likens G E. Relating nutrient uptake with transient storage in forested mountain streams[J]. Limnology and Oceanography, 2002,47(1):255-265.
[8]
Laura K L, Donald I S, Robert L B. Impact of debris dams on hyporheic interaction along a semi-arid stream[J]. Hydrological Processes, 2006,20:183-196.
[9]
Doyle M W, Stanley E H, Harbor J M. Hydrogeomorphic controls on phosphorus retention in streams[J]. Water Resources Research, 2003,39(6):1147, doi:10.1029/2003WR002038
[10]
Michael N G, Robert O H Jr, Jennifer L T. Relating transient storage to channel complexity in streams of varying land use in Jackson Hole, Wyoming[J]. Water Resources Research, 2007, 43(1), W01417, doi:10.1029/2005WR004626.
[11]
Bottacin-busolin A, Singer G, Zaramella M, et al. Effects of streambed morphology and biofilm growth on the transient storage of solutes[J]. Environ. Sci. Technol., 2009,43(19):7337-7342.
[12]
Cailin H O, Jeffery J C, Peter R W. Comparison of morphological and biological control of exchange with transient storage zones in a field-scale flume[J]. Journal of Geophysical Research, 2009, 114,G02019,doi:10.1029/2008JG000825.
Runkel R L. One-dimensional transport with inflow and storage (OTIS):A solute transport model for streams and rivers:U.S. Geological Survey Water-Resources Investigations Report, 98-4018[R]. Washington, D C:U.S. Geological Survey, 1998.
Wondzell S M. Effect of morphology and discharge on hyporheic exchange flows in two small streams in the Cascade Mountains of Oregon, USA[J]. Hydrological Processes, 2006,20(2):267-287.
[18]
Laura K L, Donald I S. The effect of transient storage on nitrate uptake lengths in streams:an inter-site comparison[J]. Hydrological Processes, 2007,21(26):3533-3548.
Weigelhofer G, Nina W, Thomas H. Limitation of stream restoration for nitrogen retention in agricultural headwater streams[J]. Ecological Engineering, 2013,60:224-234.
[21]
Argerich A, Martí E, Sabater F, et al. Influence of transient storage on stream nutrient uptake based on substrata manipulation[J]. Aquatic Sciences, 2011,73(3):365-376.
D'Angelo D J, Webster J R, Gregory S V, et al. Transient storage in Appalachian and Cascade Mountain streams as related to hydraulic characteristics[J]. Journal of the North American Benthological Society, 1993,12(3):223-235.
[24]
Jin H S, Ward G M. Hydraulic characteristics of a small Coastal Plain stream of the southeastern United States:effects of hydrology and season[J]. Hydrol. Proce., 2005,19(20):4147-4160.