1 / 12

Modeling of Critical Areas for DRP Runoff and Targeting Strategies

Modeling of Critical Areas for DRP Runoff and Targeting Strategies . Rem Confesor Jr. Research Scientist NCWQR, Heidelberg University Team Meeting # 5 Great Lakes Protection Fund Grant A Phosphorus Soil Test Metric To Reduce Dissolved Phosphorus Loading to Lake Erie July 24 , 2013.

zenia
Download Presentation

Modeling of Critical Areas for DRP Runoff and Targeting Strategies

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Modeling of Critical Areas for DRP Runoff and Targeting Strategies Rem ConfesorJr. Research Scientist NCWQR, Heidelberg University Team Meeting #5 Great Lakes Protection Fund Grant A Phosphorus Soil Test Metric To Reduce Dissolved Phosphorus Loading to Lake Erie July 24, 2013

  2. Watershed Modeling CONSTRAINTS: SPACE & TIME resolution

  3. A very simple conceptual model… Issues: One precipitation value for the whole watershed. Model is not a good representation of reality. Coefficients are unknown: need for calibration. Spatially lumped across the whole watershed, Yearly time step Precipitation Runoff flow Infiltration Yearly Runoff flow = (x)Precipitation + y(Infiltration) + Constant

  4. A little bit of improvement… Precipitation (P) Basic spatial unit Evapo- transpiration (ET) Evaporation (E) Soil storage (S) Runoff Flow (R) Infiltration (I) Lateral subsurface Flow (L) Groundwater recharge (G) S = P - ET - E - I - R; I = G + L; Discharge (Q) = (a)R + (b)L + c

  5. The hydrologic response unit (HRU)- basic spatial unit: unique combination of slope, landuse, & soil. Digital elevation model (slope/terrain) + + Land use/ crop cover Soil type Hydrologic Response Units (HRUs)

  6. The SWAT Model: • Physically-based. • Daily time step. • Long-term simulation of effects of changes in ag. management. • “RELATIVE” output changes due to these management changes. Soil Terrain Weather Flow, sediment, nutrients (N & P), etc. Agricultural practices & mgt.: tillage, fertilizer, etc. Land use/ crop cover

  7. SWAT SETUP: CROP ROTATION 2006, Corn 2007, Soybean 2008, Corn 2009, Soybean

  8. Change in DRP, lb/acre P2O5 Baseline to NoTill Baseline to NoTill + Inc

  9. Change in DRP, lb/acre P2O5 NoTill + In TO Disc Plowed + In NoTill + Bcast TO NoTill + In

  10. Change in Particulate P, lb/acre P2O5 Baseline to NoTill + In Baseline to NoTill

  11. Change in Particulate P, lb/acre P2O5 NoTill + BcastTO NoTill + In NoTill + In TO Disc Plowed + In

  12. THANK YOU! http://www.heidelberg.edu/academiclife/distinctive/ncwqr Rem Confesor rconfeso@heidelberg.edu 419-448-2204

More Related