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Stormflow Nutrient Concentrations in Coastal Streams Tributary to the Santa Barbara Channel, California: A Common Urban Response Al Leydecker, Tim Robinson and John Melack Bren School of Environmental Science, University of California, Santa Barbara; e-mail: [email protected] The catchments vary in area, topography, vegetation, soils, geology and land use, and display a wide range of base- and storm-flow nutrient concentrations. Arroyo Hondo is relatively pristine, Mission densely urban along the coastal plain, and Franklin highly 1 10 100 1000 1-O ct 30-N ov 29-Jan 30-M ar 29-M ay 28-Jul 26-S ep outflow (cf M ission C reek @ R ocky N ook 1 10 100 1000 10000 Franklin Mission A.H ondo nitrate (µ baseflow storm flow 1 10 100 Franklin Mission A.H ondo phosphate (µM baseflow storm flow 0 2 4 6 8 10 3-M ar 5-M ar 7-M ar 9-M ar NH 4 + (µM) 0 2 4 6 8 10 stage (f (a) 0 2 4 6 8 10 0 200 400 600 flow (cfs) NH 4 + (µM) 0 20 40 60 80 100 120 140 3-M ar 5-M ar 7-M ar 9-M ar NO 3 - (µM) 0 1 2 3 4 5 6 7 stage (f (b) 0 20 40 60 80 100 120 0 200 400 600 800 flow (cfs) NO 3 - (µM) 0 5 10 15 20 25 3-Mar 5-M ar 7-M ar 9-M ar PO 4 3+ (µM) 0 1 2 3 4 5 6 7 stage (f (c) 0 5 10 15 20 25 0 200 400 600 800 flow (cfs) PO 4 3+ (µM) The stormflow response of “non-urban” streams varies, but streams with appreciable urban sub-catchments in their lower basins exhibit a common pattern: (a) ammonium declines exponentially after a peak at the beginning of storms, (b) the rise and fall of nitrate concentrations are 180 degrees out of phase with the hydrograph, and (c) variations in phosphate concentrations are in parallel with the hydrograph. Concentration-discharge relationships for the urban streams show hysteresis and fit a 3-compartment baseflow/surface- flow/soilwater model. The pattern for each species is different in shape and temporal variation, indicating the lack of a common source or hydrologic response. The inference is that high ammonium concentrations are produced by early surface-flow flushing of urban surfaces, high soilwater concentrations produce the highest nitrate concentrations late on the receding storm hydrograph, and phosphate is characterized by a “flashy” urban effect (note how phosphate leads the rising hydrograph limb and lags the falling limb) superimposed on an overall catchment response. (data from 2001: (a) Mission Creek {MC00}, (b) and (c) Arroyo Burro) The relative export associated with urban streams was consistent: phosphate export at least 5-times that of ammonium, , nitrate at least 5-times that of phosphate. Export on the rising hydrograph limb was most important for ammonium (where 30 to 50 % of the ammonium is lost), somewhat important for phosphate (~25 % of total export) and relatively unimportant for nitrate (10 to 0 20 40 60 80 100 120 4-M ar 5-M ar 6-M ar 7-M ar 8-M ar 9-M ar cumulative export (kmol, cmol f 4 ) 0 200 400 600 800 flow (cf NH4 NO3 PO4 peak stage atM ontecito S t. The watersheds are steep and short, and have a rapid, “flashy” response to rainfall. The climate is Mediterranean with dry summers and approximately 20 inches of winter rainfall. Ninety % of the annual runoff occurs in less than 30 days, the majority of nutrient export takes place within 7 days. (data: MC06, 2000-2001) Santa Barbara C hannel 10 0 10 km N orth Arroyo H ondo Arroyo Burro Mission Creek PointC onception Ventura River C arpinteria Santa Monica Franklin Santa C lara R iverBasin Santa Barbara C hannel 10 0 10 km N orth Arroyo H ondo Arroyo Burro Mission Creek PointC onception Ventura River C arpinteria Santa Monica Franklin Santa C lara R iverBasin CA NV SBC LTER 1 2 3 4 5 We have been sampling nutrient concentrations in coastal streams as part of the Santa Barbara Coastal LTER. The ultimate goal is to determine nutrient export to the Santa Barbara Channel and to model how export varies with land use. We are using two approaches: (1) sampling, at their outflow, streams that represent different dominant land uses; and (2) sampling at land use transitions in a subset of selected streams. (photos counterclockwise from the upper left: a chaparral catchment with extensive oil development; the Arroyo Burro gauging station {20 have been installed to date}; the Carpinteria area from the estuary; a forested undeveloped catchment in flood; the concrete channel of Franklin Cr.; Mission Cr. in flood) This winter we are sampling storms “along the line of flow” to determine how concentrations change with land use in selected streams. During the first storm of the year, nitrate concentrations from early surface runoff increased downstream in Mission Creek, coincident with increasing residential densities (MC07 to MC06 to MC01). The greatest increase in nitrate occurred below a series of urban parks between MC06 and MC01. Interestingly, the lowest section of the stream, which flows through downtown Santa Barbara, produced a decrease in nitrate concentrations (MC00); “lawns and dogs” may contribute more nitrate than the flushing of impervious surfaces. For this small storm, where urban runoff predominated, only MC00 produced the characteristic 6 H51C-0347 sam ple site rain gauge M ission C r. urban agriculture chaparral forest riparian M C 06 M C 07 M C 01 M C 00 0 1k 0 100 200 300 400 500 30-O ct 31-O ct nitrate (µM ) 0.0 0.5 1.0 1.5 flow (cfs)orstage (ft) M C 00 M C 01 M C 06 M C 07 flow @ M C 06 stage @ M C 00 sam ple site rain gauge M ission C r. urban agriculture chaparral forest riparian M C 06 M C 07 M C 01 M C 00 0 1k

Stormflow Nutrient Concentrations in Coastal Streams Tributary to the Santa Barbara Channel, California: A Common Urban Response Al Leydecker, Tim Robinson

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Page 1: Stormflow Nutrient Concentrations in Coastal Streams Tributary to the Santa Barbara Channel, California: A Common Urban Response Al Leydecker, Tim Robinson

Stormflow Nutrient Concentrations in Coastal Streams Tributary to the Santa Barbara Channel, California: A Common Urban Response

Al Leydecker, Tim Robinson and John Melack Bren School of Environmental Science, University of California, Santa Barbara; e-mail: [email protected]

The catchments vary in area, topography, vegetation, soils, geology and land use, and display a wide range of base- and storm-flow nutrient concentrations. Arroyo Hondo is relatively pristine, Mission densely urban along the coastal plain, and Franklin highly impacted by “green house” agriculture. (data: winter 2001)

1

10

100

1000

1-Oct 30-Nov 29-Jan 30-Mar 29-May 28-Jul 26-Sep

ou

tflo

w (

cfs)

Mission Creek @Rocky Nook

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10000

Franklin Mission A. Hondo

nit

rate

M)

baseflowstormflow

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Franklin Mission A. Hondo

ph

osp

hat

e (µ

M)

baseflowstormflow

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10

3-Mar 5-Mar 7-Mar 9-Mar

NH

4+ (

µM

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ge

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)

(a)

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NH

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µM

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3-Mar 5-Mar 7-Mar 9-Mar

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t)

(b)

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)

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t)

(c)

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PO

43+ (

µM

)

The stormflow response of “non-urban” streams varies, but streams with appreciable urban sub-catchments in their lower basins exhibit a common pattern: (a) ammonium declines exponentially after a peak at the beginning of storms, (b) the rise and fall of nitrate concentrations are 180 degrees out of phase with the hydrograph, and (c) variations in phosphate concentrations are in parallel with the hydrograph.

Concentration-discharge relationships for the urban streams show hysteresis and fit a 3-compartment baseflow/surface-flow/soilwater model. The pattern for each species is different in shape and temporal variation, indicating the lack of a common source or hydrologic response. The inference is that high ammonium concentrations are produced by early surface-flow flushing of urban surfaces, high soilwater concentrations produce the highest nitrate concentrations late on the receding storm hydrograph, and phosphate is characterized by a “flashy” urban effect (note how phosphate leads the rising hydrograph limb and lags the falling limb) superimposed on an overall catchment response. (data from 2001: (a) Mission Creek {MC00}, (b) and (c) Arroyo Burro)

The relative export associated with urban streams was consistent: phosphate export at least 5-times that of ammonium, , nitrate at least 5-times that of phosphate. Export on the rising hydrograph limb was most important for ammonium (where 30 to 50 % of the ammonium is lost), somewhat important for phosphate (~25 % of total export) and relatively unimportant for nitrate (10 to 15 %). (Mission Cr. {MC00}data, 2001)

0

20

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4-Mar 5-Mar 6-Mar 7-Mar 8-Mar 9-Mar

cu

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lati

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ol

for

NH 4

)

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200

400

600

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flo

w (

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NH4

NO3

PO4

peak stage at Montecito St.

The watersheds are steep and short, and have a rapid, “flashy” response to rainfall. The climate is Mediterranean with dry summers and approximately 20 inches of winter rainfall. Ninety % of the annual runoff occurs in less than 30 days, the majority of nutrient export takes place within 7 days. (data: MC06, 2000-2001)

Santa Barbara Channel

10 0 10 km

North

Arroyo Hondo

Arroyo BurroMission Creek

Point Conception

Ventura River

Carpinteria

SantaMonica

Franklin

Santa Clara River BasinSanta Barbara Channel

10 0 10 km

North

Arroyo Hondo

Arroyo BurroMission Creek

Point Conception

Ventura River

Carpinteria

SantaMonica

Franklin

Santa Clara River Basin

CA NV

SBC LTER

12

34

5

We have been sampling nutrient concentrations in coastal streams as part of the Santa Barbara Coastal LTER. The ultimate goal is to determine nutrient export to the Santa Barbara Channel and to model how export varies with land use. We are using two approaches: (1) sampling, at their outflow, streams that represent different dominant land uses; and (2) sampling at land use transitions in a subset of selected streams. (photos counterclockwise from the upper left: a chaparral catchment with extensive oil development; the Arroyo Burro gauging station {20 have been installed to date}; the Carpinteria area from the estuary; a forested undeveloped catchment in flood; the concrete channel of Franklin Cr.; Mission Cr. in flood)

This winter we are sampling storms “along the line of flow” to determine how concentrations change with land use in selected streams. During the first storm of the year, nitrate concentrations from early surface runoff increased downstream in Mission Creek, coincident with increasing residential densities (MC07 to MC06 to MC01). The greatest increase in nitrate occurred below a series of urban parks between MC06 and MC01. Interestingly, the lowest section of the stream, which flows through downtown Santa Barbara, produced a decrease in nitrate concentrations (MC00); “lawns and dogs” may contribute more nitrate than the flushing of impervious surfaces. For this small storm, where urban runoff predominated, only MC00 produced the characteristic urban nitrate signature shown previously.

6

H51C-0347

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30-Oct 31-Oct

nit

rate

M)

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flo

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cfs)

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e (

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MC00

MC01

MC06

MC07

flow @ MC06

stage @ MC00

sample siterain gaugeMission Cr.urbanagriculturechaparralforestriparianMC06

MC07

MC01

MC00

0 1k

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30-Oct 31-Oct

nit

rate

M)

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ft)

MC00

MC01

MC06

MC07

flow @ MC06

stage @ MC00

sample siterain gaugeMission Cr.urbanagriculturechaparralforestriparianMC06

MC07

MC01

MC00

0 1k