Nutrient loads exported from managed catchments reveal emergent biogeochemical stationarity

被引:352
作者
Basu, Nandita B. [1 ]
Destouni, Georgia [2 ]
Jawitz, James W. [3 ]
Thompson, Sally E. [4 ]
Loukinova, Natalia V. [1 ]
Darracq, Amelie [2 ]
Zanardo, Stefano [5 ,6 ]
Yaeger, Mary [7 ]
Sivapalan, Murugesu [7 ,8 ,11 ]
Rinaldo, Andrea [9 ,10 ]
Rao, P. Suresh C. [5 ,6 ]
机构
[1] Univ Iowa, Dept Civil & Environm Engn, Iowa City, IA 52242 USA
[2] Stockholm Univ, Dept Phys Geog & Quaternary Geol, SE-10691 Stockholm, Sweden
[3] Univ Florida, Soil & Water Sci Dept, Gainesville, FL 32611 USA
[4] Duke Univ, Nicholas Sch Environm, Durham, NC 27701 USA
[5] Purdue Univ, Sch Civil Engn, W Lafayette, IN 47907 USA
[6] Purdue Univ, Dept Agron, W Lafayette, IN 47907 USA
[7] Univ Illinois, Dept Civil & Environm Engn, Urbana, IL 61801 USA
[8] Univ Illinois, Dept Geog, Urbana, IL 61801 USA
[9] Univ Padua, Dipartimento Ingn Idraul Marittima & Geotecn, I-35131 Padua, Italy
[10] Univ Padua, Int Ctr Hydrol Dino Tonini, I-35131 Padua, Italy
[11] Delft Univ Technol, Fac Civil Engn & Geosci, Dept Water Management, Delft, Netherlands
关键词
MISSISSIPPI RIVER-BASIN; WATER; EUTROPHICATION; DYNAMICS; HYPOXIA; DEAD; FLUX; SOIL;
D O I
10.1029/2010GL045168
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Complexity of heterogeneous catchments poses challenges in predicting biogeochemical responses to human alterations and stochastic hydro-climatic drivers. Human interferences and climate change may have contributed to the demise of hydrologic stationarity, but our synthesis of a large body of observational data suggests that anthropogenic impacts have also resulted in the emergence of effective biogeochemical stationarity in managed catchments. Long-term monitoring data from the Mississippi-Atchafalaya River Basin (MARB) and the Baltic Sea Drainage Basin (BSDB) reveal that inter-annual variations in loads (L-T) for total-N (TN) and total-P (TP), exported from a catchment are dominantly controlled by discharge (Q(T)) leading inevitably to temporal invariance of the annual, flow-weighted concentration, (C) over bar (f) = (L-T/Q(T)). Emergence of this consistent pattern across diverse managed catchments is attributed to the anthropogenic legacy of accumulated nutrient sources generating memory, similar to ubiquitously present sources for geogenic constituents that also exhibit a linear L-T-Q(T) relationship. These responses are characteristic of transport-limited systems. In contrast, in the absence of legacy sources in less-managed catchments, (C) over bar (f) values were highly variable and supply limited. We offer a theoretical explanation for the observed patterns at the event scale, and extend it to consider the stochastic nature of rainfall/flow patterns at annual scales. Our analysis suggests that: (1) expected inter-annual variations in L-T can be robustly predicted given discharge variations arising from hydro-climatic or anthropogenic forcing, and (2) water-quality problems in receiving inland and coastal waters would persist until the accumulated storages of nutrients have been substantially depleted. The finding has notable implications on catchment management to mitigate adverse water-quality impacts, and on acceleration of global biogeochemical cycles. Citation: Basu, N. B., et al. (2010), Nutrient loads exported from managed catchments reveal emergent biogeochemical stationarity, Geophys. Res. Lett., 37, L23404, doi:10.1029/2010GL045168.
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