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1937 1962 1995 Landscape controls on surface water quality
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sourcepathwaydestination Stream ecology Landscape ecology precip
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Variation in source water -Related to land use -Ionic composition (N, S) and pH
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Landscape control on surface water quality is all about… Pathway of water from land to water body –As water moves from one place to another: Physical changes –Particulate accumulation/removal –Leaching Chemical transformations (biogeochemistry) –Different patches cause different types, amounts of physical, chemical change
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source pathway destination Patch composition Patch size Patch arrangement
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Effects of pathway (landscape structure) on water quality How pathway composition varies across large areas
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Effects of landscape elements (patches) on water chemistry 1. Parent geology Variation in parent geology, weathering ---> chemical variation in water Sandstone + dolomite dolomite Mixed granites Dolomite, shale, limestone
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From: Jones, J.B. 2002. Freshwater Biology 47:971-983
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Geology/weathering effects Cations –In particular: Ca, Mg, Si Anions –Carbonates productivity, acidification risk Nutrients –Phosphorus all from rock weathering Slow rate of weathering widespread P limitation –Nitrogen Geological effects exist within, between drainages
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From: Holloway et al. 1998. Nature 395:785-788.
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Geology/weathering effects Effects of parent geology on the path that water takes –Preferential flow paths –Land forms
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Effects of landscape elements (patches) on water chemistry 2. Land Use/Land Cover Variation in land use/land cover ---> variation in water quality *Best studied landscape effect on water quality
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Land use-water quality relationships % Agriculture in the basin (Stanley unpublished)
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Signal of agricultural, urban land cover is often strong and direct –Nutrient enrichment –Classic pollutants –Organic C % agriculture But not always…
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When water quality is not predictable from land cover H 1 : Hydrologic pathways by-pass land cover
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What we see… What actually happens (Deep) groundwater sources by-passing land cover
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Hydrology + landscape ecology There are many ways for water to flow downhill
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When water quality is not predictable from land cover H 2 : Flowpaths vary as a function of landscape position –Water quality varies among lakes despite similar land cover Different lakes fed by water from different sources
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Landscape position related to lake hydrology Precipitation Input Groundwater Input “Highland” lake “Lowland” lake
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High (little GW) Low (lots of GW) 5 10 100 200 300 50 Cond (µS cm -1 ) Landscape position 40 20 10 5 1 Chl a (µ g L -1 ) Landscape position High (little GW) Low (lots of GW) From: Riera et al. 2000. Freshwater Biology 43:301-318
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When water quality is not predictable from land cover H 3 : Hot spot effects –Patches that have a disproportionately large influence on water quality Addition of particles, solutes Removal of particles, solutes
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Hot spots 1. Sites where water moves quickly from land to lake/stream
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P derived from small hotspots (“effective areas”) Extent of hotspots affected by land use –Urban cover accounts for: 10% of cover 20-55% of P input to L. Mendota From:Soranno et al. 1996 Ecological Applications 6:865-878
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Hot spots 2. Sites where water is subject to distinct physical/biogeochemical environment, intensive change ecotones
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Riparian zones Aquatic/terrestrial interface –Soils often saturated (anoxic), rich in OM –Water velocity slows Rapid bgc change, particle trapping NO 3 -N (ug/L) UP RM RO
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Riparian zones Solution to non-point source pollution? –Sometimes… May or may not be effective in reducing nutrient loads in groundwater –Pathways –Size, shape of RZ
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The challenge- determining when water does/does not pass through the riparian zone
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Spatial configuration of riparian zone affects nutrient retention From: Weller et al. 1998. Ecological Applications 8:1156-1169
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Landscape influence on water quality determined by: -Relative importance of different flowpaths -What happens along these flow path - Lots of research opportunities for questions re: -patch arrangement, patch size precip deep gw
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