Agronomy Journal Volume 103, Issue 3 2011 899
Soil Fertility & Crop Nutrition
Incorporation of Municipal Biosolids Affects Organic Nitrogen
Mineralization and Elephantgrass Biomass Production
Miguel S. Castillo, Lynn E. Sollenberger,* João M. B. Vendramini, Kenneth R. Woodard,
George A. O’Connor, Maria L. Silveira, and Jerry B. Sartain
Published in Agron. J. 103:899–905 (2011)
Published online 28 Mar 2011
doi:10.2134/agronj2010.0497
Copyright © 2011 by the American Society of Agronomy, 5585 Guilford
Road, Madison, WI 53711. All rights reserved. No part of this periodical may
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mechanical, including photocopying, recording, or any information storage
and retrieval system, without permission in writing from the publisher.
A
dequate nutrient supply is necessary to meet the
requirements of high-yielding bioenergy crops. Land applica-
tion of MBS has been shown to be an efective alternative for
reducing the amount of inorganic fertilizer used in bioenergy crop
production systems (Heller et al., 2003; Castillo et al., 2010b). Use
of MBS also recycles nonrenewable resources and addresses the
problem of inding alternative options for MBS disposal.
Like many other organic sources of nutrients, when MBS is
applied on an N-rate basis there is potential for overapplication
of P due to the narrower N:P ratio in MBS vs. plant require-
ments. Typical concentrations of total N and P in MBS range
from 35 to 68 and 18 to 39 g kg
–1
, respectively (USEPA, 1999).
hus, in some cases application of MBS is limited to P-based
rates. Another issue of signi icance when using MBS is that
~800 g kg
–1
of the total N is in organic forms (Sommers, 1977;
Binder et al., 2002), meaning that this N is not immediately
available for plant uptake. Plant-available nitrogen (PAN) in
MBS is a function of the initial inorganic N concentration
(NH
4
–N and NO
3
–N) and the proportion of organic N that
mineralizes over time (Gilmour and Skinner, 1999).
Organic N mineralization occurs through the activity of
nonspeciic heterotrophic soil microorganisms (Jarvis et al.,
1996; Pierzynski et al., 2000; He et al., 2003). he rate and
quantity of mineralization largely depends on the quantity and
composition of the organic matter (Sommers et al., 1981) and the
inluence of the environment on biological activity (Goncalves
and Carlyle, 1994; Castillo et al., 2010a). hus, placement of the
organic substrate (soil-incorporated vs. surface-applied), results
in diferences in microenvironmental conditions (e.g., contact of
MBS with moist soil particles and microbes) and may inluence
the dominant forms of N (NH
4
–N vs. NO
3
–N) and rates of
organic-N mineralization (Terry et al., 1978; Clark and Gilm-
our, 1983; Gilmour and Clark, 1988; He et al., 2003).
Experiments with poultry litter and cattle manure have
demonstrated beneits of soil incorporation. hese include
reduction in N volatilization losses, odors, and residue cover as
well as an increase in organic N mineralization and crop yields
(Hanna et al., 2000; Pote et al., 2003; Sharpe et al., 2004).
Several laboratory incubation studies have demonstrated the
positive efects of incorporation of organic materials produced
in wastewater treatment plants (King, 1973; Terry et al., 1978;
Sommers et al., 1981; Adamsen and Sabey, 1987; He et al.,
2003). Fewer data have been reported from actual ield-incuba-
tion trials (He et al., 2000; Hanselman et al., 2004) and from
studies that have measured plant responses (e.g., DM yield) as
an indicator of organic N mineralization.
Although soil incorporation as a nutrient management
practice has been studied and recommended for a variety of
organic and inorganic sources, little attention has been given to
the efect of incorporation of MBS on plant DM yield. hus,
two experiments were conducted under ield conditions to
assess the efects of incorporation of Class A MBS on plant and
soil responses and on decomposition and organic N mineraliza-
tion rates of MBS. he objectives of Exp. 1 were to: (i) quantify
ABSTRACT
Municipal biosolids (MBS) represents an alternative source of nutrients for the production of bioenergy crops like elephantgrass
(Pennisetum purpureum Schum.). Two experiments were conducted during 2 yr in Florida to evaluate the efect of soil incorporation
vs. surface application of MBS on: (i) elephantgrass dry matter (DM) yield, tissue N and P concentration and removal, and soil C and
P (Exp. 1); and (ii) organic N mineralization and DM decomposition rates of MBS measured in the ield using a litter bag incubation
technique (Exp. 2). In Exp. 1, three treatments supplied 350 kg total N ha
–1
yr
–1
from surface-applied municipal biosolids (MBS-
SA), soil-incorporated municipal biosolids (MBS-INC), and surface-applied ammonium nitrate (NH
4
NO
3
). A fourth treatment
provided 700 kg total N ha
–1
yr
–1
from MBS-SA (double rate of municipal biosolids, 2x-MBS). In Exp. 2, MBS was ield incubated
in litter bags placed on the soil surface or at a 5-cm soil depth. Elephantgrass DM yield, and N and P removal were greater for MBS-
INC than MBS-SA. Dry matter yield for MBS-INC was not diferent than for NH
4
NO
3
fertilizer (22.5 vs. 24.3 Mg ha
–1
). Removal
of N and P increased 39 and 10 kg ha
–1
yr
–1
, respectively, for MBS-INC and MBS-SA. Total organic N mineralized was greater for
MBS-INC (386 g kg
–1
) than MBS-SA (308 g kg
–1
). Incorporation of MBS increases elephantgrass DM yield and nutrient removal
compared to surface application and allows MBS to replace a greater proportion of inorganic N fertilizer.
M.S. Castillo, L.E. Sollenberger, and K.R. Woodard, Agronomy Dep., Univ.
of Florida, Gainesville, FL 32611-0500; J.M.B. Vendramini and M.L. Silveira,
Range Cattle Research and Education Center, Ona, FL 33865; G.A. O’Connor
and J.B. Sartain, Soil and Water Science Dep., Univ. of Florida, Gainesville, FL
32611. Received 7 Dec. 2010. *Corresponding author (lesollen@ul.edu).
Abbreviations: BDR, biosolids decomposition rate; DM, dry matter; MBS,
municipal biosolids; MBS-INC, municipal biosolids, soil incorporated; MBS-SA,
municipal biosolids, surface applied; 2x-MBS, double rate of municipal biosolids;
NMR, nitrogen mineralization rate; WEP, water-extractable phosphorus.