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a SimBiotic Software, 407 E. Main St., Missoula, MT 59802
b School of Life Sciences, Arizona State Univ., P.O. Box 874501, Tempe, AZ 85287. Research was performed at Arizona State University
* Corresponding author (nbgrimm{at}asu.edu).
Received for publication April 24, 2008. In the Central Arizona–Phoenix (CAP) ecosystem, managers divert mixed stream water and groundwater to maintain an artificial lake chain in Indian Bend Wash (IBW), a historically flashy, ephemeral, desert stream. Nutrient concentrations in the CAP ecosystem's groundwater, stream water, and floodwater differ: stream water has low concentrations of both inorganic N and P, while groundwater is low in inorganic P but rich in nitrate (NO3–). Consequently, groundwater contribution drives inorganic N concentrations in the lake chain. In contrast, floodwater typically has high P concentrations while remaining low in N. Thus we expected N and P concentrations in IBW lakes to vary with the mix of water flowing through them. Elevated NO3– and low inorganic P concentrations were predicted when groundwater pumping was pronounced and this prediction was supported. We hypothesized that these predictable changes in water chemistry would affect nutrient limitation of phytoplankton. Laboratory nutrient-addition bioassays demonstrated that phytoplankton growth was P-limited throughout the summer of 2003 when N/P was high. However, after a late-season flood drove N/P below 31:1, the expected threshold between N and P limitation, N limitation was observed. Our results indicate that effects of floods, the preeminent historic drivers of Sonoran Desert stream biogeochemistry, are mitigated in urban ecosystems by decisions about which spigots to turn. Consequently, nutrient limitation of urban streams is driven as much by management decisions as by natural hydrologic variation.
Abbreviations: CAP, Central Arizona–Phoenix DIN, dissolved inorganic nitrogen, which is the sum of ammonium and nitrate IBW, Indian Bend Wash L-1, L-2, L-3, L-4, L-5, L-6, L-7, & L-8, consecutive artificial lakes along Indian Bend Wash (from upstream to downstream) N, nitrogen NH4+, ammonium NO3–, combined nitrate and nitrite N/P, molar ratio of dissolved inorganic nitrogen to soluble reactive phosphorus N0 and Nt, in-vivo fluorescence of phytoplankton incubation at time 0 and time t r, exponential growth rate Qmax, maximum average daily discharge during flood event Roos. Well, a groundwater well located on Roosevelt Street delivering water directly to Indian Bend Wash SRP, soluble reactive phosphorus TDP, total dissolved phosphorus
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