Role of rainfall intensity and hydrology in nutrient transport via surface runoff

Peter J A Kleinman, M. S. Srinivasan, Curtis James Dell, John P. Schmidt, Andrew N. Sharpley, Ray B. Bryant

Research output: Contribution to journalArticle

101 Citations (Scopus)

Abstract

Loss of soil nutrients in runoff accelerates eutrophication of surface waters. This study evaluated P and N in surface runoff in relation to rainfall intensity and hydrology for two soils along a single hillslope. Experiments were initiated on 1- by 2-m plots at foot-slope (6%) and mid-slope (30%) positions within an alfalfa (Medicago sativa L.)-orchardgrass (Dactylis glomerata L.) field. Rain simulations (2.9 and 7.0 cm h-1) were conducted under wet (spring) and dry (late-summer) conditions. Elevated, antecedent sol moisture at the foot-slope during the spring resulted in less rain required to generate runoff and greater turn-off volumes, compared with runoff from the well-drained mid-slope in spring and at both landscape positions in late summer. Phosphorus in runoff was primarily in dissolved reactive form (DRP averaged 71% of total P), with DRP concentrations from the two soils corresponding with soil test P levels. Nitrogen in runoff was mainly nitrate (NO3-N averaged 77% of total N). Site hydrology, not chemistry, was primarily responsible for variations in mass N and P losses with landscape position. Larger runoff volumes from the foot-slope produced higher losses of total P (0.08 kg ha-1) and N (1.35 kg ha-1) than did runoff from the mid-slope (0.05 total P kg ha-1; 0.48 kg N ha-1), particularly under wet, spring-time conditions. Nutrient losses were significantly greater under the high intensity rainfall due to larger runoff volumes. Results affirm the critical source area concept for both N and P: both nutrient availability and hydrology in combination control nutrient loss.

Original languageEnglish (US)
Pages (from-to)1248-1259
Number of pages12
JournalJournal of Environmental Quality
Volume35
Issue number4
DOIs
StatePublished - Jul 1 2006

Fingerprint

Hydrology
precipitation intensity
Runoff
Nutrients
Rain
hydrology
runoff
nutrient
Soils
Springs (water)
nutrient loss
Eutrophication
soil test
summer
Sols
alfalfa
hillslope
nutrient availability
Surface waters
soil nutrient

All Science Journal Classification (ASJC) codes

  • Environmental Engineering
  • Water Science and Technology
  • Waste Management and Disposal
  • Pollution
  • Management, Monitoring, Policy and Law

Cite this

Kleinman, P. J. A., Srinivasan, M. S., Dell, C. J., Schmidt, J. P., Sharpley, A. N., & Bryant, R. B. (2006). Role of rainfall intensity and hydrology in nutrient transport via surface runoff. Journal of Environmental Quality, 35(4), 1248-1259. https://doi.org/10.2134/jeq2006.0015
Kleinman, Peter J A ; Srinivasan, M. S. ; Dell, Curtis James ; Schmidt, John P. ; Sharpley, Andrew N. ; Bryant, Ray B. / Role of rainfall intensity and hydrology in nutrient transport via surface runoff. In: Journal of Environmental Quality. 2006 ; Vol. 35, No. 4. pp. 1248-1259.
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Kleinman, PJA, Srinivasan, MS, Dell, CJ, Schmidt, JP, Sharpley, AN & Bryant, RB 2006, 'Role of rainfall intensity and hydrology in nutrient transport via surface runoff', Journal of Environmental Quality, vol. 35, no. 4, pp. 1248-1259. https://doi.org/10.2134/jeq2006.0015

Role of rainfall intensity and hydrology in nutrient transport via surface runoff. / Kleinman, Peter J A; Srinivasan, M. S.; Dell, Curtis James; Schmidt, John P.; Sharpley, Andrew N.; Bryant, Ray B.

In: Journal of Environmental Quality, Vol. 35, No. 4, 01.07.2006, p. 1248-1259.

Research output: Contribution to journalArticle

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Kleinman PJA, Srinivasan MS, Dell CJ, Schmidt JP, Sharpley AN, Bryant RB. Role of rainfall intensity and hydrology in nutrient transport via surface runoff. Journal of Environmental Quality. 2006 Jul 1;35(4):1248-1259. https://doi.org/10.2134/jeq2006.0015