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Utilizing Stable Isotopes and Spatial Analysis to Understand Hillslope Ecohydrological.

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Figure

Figure 2.1: Study site topography and infrastructure. Triangles (▲Table 2.2. Circles (the northeast towards the tributary, with the steepest gradient northeast of the lagoons (NC Floodplain MappingProgram, 2011)
Figure 2.2: Composite kriged surface with groundwater flow direction and all tree foliar δsmall and large trees (July 2010), waste application field pines (October 2010), and boundary samples collected inJune 2011
Figure 2.3: Photosynthetically active radiation measured .6km south of study site atState Climate Office of North Carolina weather station CLA2 (35.59158 -78.45889) June2012
Figure 2.4: Daily evaporation from open water measured .6km south of study site atState Climate Office of North Carolina weather station CLA2 (35.59158 -78.45889) June2012
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