Title page for ETD etd-02202009-103316


Type of Document Dissertation
Author Arellano Ogaz, Eduardo
Author's Email Address earellan@uc.cl
URN etd-02202009-103316
Title Changes in Soil Nitrogen Following Biosolids Application to Loblolly Pine (Pinus Taeda L.) Forest in the Virginia Piedmont
Degree PhD
Department Forestry
Advisory Committee
Advisor Name Title
Fox, Thomas R. Committee Chair
Aust, Wallace Michael Committee Member
Burger, James A. Committee Member
Daniels, Walter Lee Committee Member
Evanylo, Gregory K. Committee Member
Keywords
  • forest fertilization
  • Nitrogen leaching
  • Nitrogen mineralization
  • biosolids
  • Loblolly pine (Pinus Taeda L.)
Date of Defense 2009-01-12
Availability unrestricted
Abstract
Application of biosolids as an alternative source of Nitrogen (N) is becoming a common silviculture practices on loblolly pine forest. However, little is known about how biosolids type, application rate, and timing affect forest floor and soil N availability in pine plantations. The objectives of this study were to determine the effect of different types, rates, and season of application of biosolids on forest floor and soil N. The study was established in a 17-year-old loblolly pine plantation in Amelia County, VA. Anaerobically digested (AD225), lime stabilized (LS225), and pelletized (Pellet225) biosolids and a conventional inorganic urea plus diammonium phosphate fertilizer (U+DAP225) were surface applied at a rate of 225 kg ha-1 based on Plant Available Nitrogen (PAN) between March 5th and 10th, 2006. Anaerobically digested biosolids were also surface applied at the rates of 900 kg PAN ha-1 and 1800 kg PAN ha-1 (AD900 and AD1800). Anaerobically digested biosolids at the rate of 900 kg PAN ha-1 were also applied on November 5th, 2005 (AD900F).

Surface application of different type of biosolids in a loblolly pine plantation increased soil N availability and mineralization when biosolids were applied at the permitted rate of 225 kg PAN ha-1. Surface soil NH4-N and NO3-N availability and N mineralization was significantly different among biosolids type over time. N release from different type of biosolids depends on the initial inorganic N content, and N mineralization in biosolids. The average soil N availability and mineralization was significantly greater in the Pellet225 treatments than in all the other treatments. Soil N availability decreased in winter in all the treatments but remained generally higher than the control until the end of the second growing season. Nitrate-N concentrations in lysimeters were below water quality standard limits in all the treatments applied at the rate of 225 kg PAN ha-1. Accumulation of N, C, and Ca in the forest floor was well correlated with the amount of biosolids applied on each treatment. The surface application of different type of biosolids had minimal impact upon total N and C in the mineral soil. Increasing application rates of anaerobically digested biosolids directly increased soil N availability and mineralization. Nitrate-N concentrations in lysimeters were above water quality standards limits during several months in the AD900 and AD1800 treatments. Significant differences in the forest floor total N, C and Ca were observed with increasing application rates of biosolids. Total C accumulation was significantly higher in the forest floor in the AD1800 treatment. However, we observed no effect on soil total C with increasing application rates of biosolids. We found that biosolids application during spring significantly increased soil extractable N, N mineralization, NO3-N leaching, and total C in the mineral soil in comparison to the fall application. Fall application significantly increased NH4-N leaching and soil extractable Ca. We observed no significant effect on ion exchangeable N measured on membranes, total N, C, Ca, and pH measured in the forest floor, and soil total N and pH in the mineral soil. Our results demonstrated that permitted surface application of biosolids at the rate of 225 kg PAN ha-1 in a loblolly pine plantation increased surface soil N availability without increasing the potential for NO3-N groundwater pollution.

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