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a Washington State Univ. Puyallup Research and Extension Center, 7612 Pioneer Way E., Puyallup, WA 98371-4998
b Dep. of Crop and Soil Sci., Oregon State Univ., Corvallis, OR 97331
* Corresponding author (cogger{at}wsu.edu).
| ABSTRACT |
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Abbreviations: PAN, plant available nitrogen
| INTRODUCTION |
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In the 1980s, the USEPA developed guidelines for estimating mineralization of organic N based on the type of biosolids processing (USEPA, 1983). The USEPA recommended a mineralization rate of 20% of biosolids organic N the first year after application for anaerobically digested biosolids, and 30% for aerobically digested biosolids. Second-year mineralization estimates were 10% for anaerobic and 15% for aerobic biosolids. Data from laboratory mineralization experiments by Parker and Sommers (1983) and King (1984) supported those first-year estimates of N availability. Subsequent field studies have suggested greater N availability for anaerobically digested biosolids (Sullivan et al., 1997; Cogger et al., 1999). Little data has been available for other types of biosolids.
Field studies are a less-controlled but more agronomically realistic approach for assessing biosolids N availability. Nitrogen uptake by a field crop fertilized with biosolids can be compared with N uptake from the same crop fertilized with inorganic N to estimate the amount of plant available N derived from the biosolids during the growing season. Intensively managed, irrigated forage grass is an ideal crop for evaluating PAN. Forage grass has a linear response to N application across a wide range of rates during a long growing season (Whitehead, 1995), with little residual left in the soil, even at available N rates of 300 kg ha1 or more (Steenvoorden et al., 1986; Cogger et al., 1999). In addition, forage grasses are harvested multiple times during the growing season, allowing evaluation of N availability across time.
To improve our ability to predict N availability from biosolids produced by a variety of treatment processes, we conducted a field N recovery experiment with irrigated tall fescue. Our specific objective was to assess the effect of biosolids processing on plant-available N in the first and second growing seasons after biosolids application.
This experiment was part of a national biosolids N availability assessment project. Summary data from the first year after biosolids application was combined with laboratory incubations, field data from several other locations across the USA, and model simulations to develop national estimates for biosolids N availability (Gilmour et al., 2000; Gilmour et al., 2003).
| MATERIALS AND METHODS |
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The climate is typical of the maritime Pacific Northwest, with cool, wet winters and mild, dry summers. Mean annual temperature is 11°C with a January mean of 4°C and a July mean of 18°C. Mean annual precipitation is 1020 mm, falling mostly as rain between October and May. Irrigation is necessary to maintain intensive forage production during the dry summer months. During the study period, precipitation for April through October was 188 mm in 1998, 228 mm in 1999, and 300 mm in 2000. The precipitation was supplemented by 285 mm of sprinkler irrigation in 1998, 280 mm in 1999, and 175 mm in 2000.
Forage-type tall fescue AU Triumph was planted in June 1996 on ground that was previously cropped to silage corn (Zea mays L.). The tall fescue was maintained with inorganic fertilizers and irrigation until the experimental treatments were applied in May 1998 (Exp. 1) or May 1999 (Exp. 2). Tall fescue was harvested and removed from the plots six times per year during the establishment period and twice (April and May) before biosolids were applied in the first experimental year.
Biosolids
We obtained biosolids from 14 wastewater treatment plants (Table 1). The biosolids represented a range of wastewater plant sizes and biosolids treatment processes, including aerobic and anaerobic mesophilic digestion, thermophilic digestion, lime stabilization, lagooning, dewatering, air drying, and heat drying. All of the biosolids used were dewatered or dried materials. Solids content of the biosolids was determined on triplicate samples by drying at 60°C. Biosolids NH4 and NO3 were extracted with 1 M KCl. Ammonium-N was determined by automated colorimetric analysis with the salicylate method and NO3N by cadmium reduction (Mulvaney, 1996). Nitrate-N was less than the detection limit of 0.01 mg kg1 in all biosolids samples in 1998, and NO3 analyses were not run in 1999. Biosolids total N and C were determined with a LECO Total CNS 2000 elemental analyzer (Nelson and Sommers, 1996).
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Experiment 1 (1998-1999) included biosolids from eight sources (Table 1), five inorganic N treatments and a zero-N control. On 6 May 1998, a single surface application of each type of biosolids was made to the appropriate plots in Exp. 1. The target application rate was 400 to 500 kg total biosolids N per hectare. At this target rate, the expected plant available N would be well within the linear portion of the N uptake curve for intensively managed forage grass (Whitehead, 1995). Before applying the biosolids, the tall fescue was cut at a 5-cm height and the harvested forage removed. The biosolids were not incorporated.
The five inorganic N treatments received a total of 50, 100, 150, 200, and 250 kg N ha1 in 1998 as ammonium nitrate (34-0-0 N-P-K). The inorganic N was split into three equal applications; one on the same date as the biosolids application, and the remaining two following the June and July harvests.
The tall fescue was harvested at the early boot stage with a small plot forage harvester. A 1- x 6-m swath was harvested from each plot at a 5-cm height. Harvests were on 3 June, 6 July, 5 August, 14 September, and 23 October. Because the tall fescue was harvested twice in 1998 before the biosolids application, the first harvest of the experiment was actually the third harvest of the season. The harvested forage from each plot was weighed wet, and a 500-g subsample was collected and oven-dried (60°C) for determination of dry matter and total N (LECO CNS 2000).
No biosolids were applied to Exp. 1 in 1999, but the tall fescue was harvested in the same manner as in 1998 to measure N uptake in the second year following biosolids application. The biosolids treatments received 150 kg ha1 N as 34-0-0 split across five applications (one in March and the others following each of the first four harvests) to maintain stand vigor because greatly reduced N mineralization was expected during the second year. The five inorganic N treatments received 34-0-0 at rates ranging from 75 to 375 kg N ha1 split across the same five application dates. Plots were harvested on 22 April, 24 May, 21 June, 21 July, 24 August, and 4 October. All other procedures were the same as in 1998.
Experiment 2 (1999-2000) included biosolids from nine sources (Table 1), four inorganic N treatments and a zero-N control. Three of the biosolids came from sources included in Exp. 1 (Baltimore, Everett, and Stayton), while the other six came from different wastewater treatment plants. The biosolids from Baltimore and Stayton were fresh material in 1999, while the Everett biosolids (long-term lagoon material) came from the same stockpile that was used in 1998. The biosolids were applied to freshly harvested plots on 25 and 28 May 1999. The four inorganic N treatments received ammonium nitrate at rates of 50, 100, 150, and 200 kg N ha1, split into three equal applications. Plots were harvested on 21 June, 21 July, 24 August, and 4 October.
In 2000, the biosolids treatments received 150 kg N ha1 as 34-0-0 and the inorganic N treatments received 75, 150, 225, or 300 kg N ha1 as 34-0-0. All applications were split across five dates, the same as for Exp. 1. Harvest dates for 2000 were 12 April, 22 May, 21 June, 20 July, 24 August, and 4 October. All other procedures were the same as for Exp. 1.
Statistical Analyses and Calculations
Statistics for yield and N uptake were computed by ANOVA and Duncan's Multiple Range procedures (SAS Institute, 1996). Means were compared with Duncan's test following a protected (P < 0.05) F test.
Biosolids PAN was estimated by a two-step calculation. First, we used linear regression to calculate the fertilizer efficiency coefficient for the inorganic N treatments:
![]() | [1] |
Separate fertilizer efficiency regressions were calculated for each experiment each year. Year 2 regressions were calculated with and without the first harvest (April) of the year. Then the equation was rearranged and biosolids PAN calculated. For Year 1,
![]() | [2] |
![]() | [3] |
| RESULTS AND DISCUSSION |
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Tall fescue N uptake for the inorganic N treatments had a linear response both years (Exp. 1 shown in Fig. 1) , validating the use of the linear regression model to calculate fertilizer N efficiency and plant available N. All of the inorganic N uptake data sets fit the linear model well (Table 4).
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Others have also reported rapid N availability from heat-dried biosolids in field trials (Goatley et al., 1998; Muchovej and Rechcigl, 1998). In 60-d laboratory incubations, Smith and Durham (2002) assessed the effect of heat drying on biosolids N release. Despite the loss of NH4 from heat drying, they found that heat drying increased the rate of incubation N release in three of five biosolids tested. Mineralizable N increased for all of the biosolids.
Plant Available NitrogenYear 2
Biosolids PAN was much less in Year 2 than in Year 1, although it was still substantial for most of the materials (Table 6). PAN from lagoon biosolids were generally lower than for the other materials, ranging from apparent immobilization for Everett to 8% of total N for Iona. The heat-dried materials also had low second-year PAN (5 to 8%). This indicates that after the initial period of rapid N release from heat-dried biosolids, subsequent N release is slow. Most of the dewatered and air-dried nonlagoon biosolids had Year 2 PAN ranging from 10 to 14% of total biosolids N, with the material from Bingen at 17% (Table 6). This second-year PAN is large enough to affect N application decisions for many crops.
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We did not measure NH3 volatilization in this project, nor did we attempt to separate the contributions of organic and NH4N to PAN. Organic N was the predominant N form in all of the biosolids. All 14 biosolids had <25% of total N in NH4 form, and eight had <10% as NH4. With surface application of dewatered materials, significant NH3 loss is expected. It is interesting to note that biosolids that produced the greatest proportion of early season tall fescue N uptake (Stayton, Milwaukee, Baltimore) had low concentrations of NH4N (Table 1). These results suggest that NH4 was a minor contributor to PAN in this study.
Summary and Implications for Biosolids Managers
The results of this study showed that first-year PAN was similar across a range of biosolids treatment processes. Lagoon biosolids were the exception. The PAN for Year 1 was 37 ± 5% averaged across all nonlagoon biosolids, which is higher than predicted with the standard USEPA guidelines (USEPA, 1983). The PAN from lagoon biosolids varied from 8 to 25%, depending on the age of the material. In the second year, PAN for heat-dried biosolids was lower than for dewatered and air-dried materials. Total Year 2 PAN for dewatered and air-dried nonlagoon biosolids was 13 ± 2%, while Year 2 PAN for heat-dried biosolids was about half as large. It appears that heat drying increases the short term availability of biosolids N, but decreases long term N availability.
Biosolids producers, users, and regulators can employ this information in developing biosolids application plans for a similar range of materials in similar climates. If biosolids are used in a summer annual cropping system, more than half of the expected second-year PAN may be susceptible to leaching before it is taken up by the crop. Timely planting of an N-scavenging cover crop during the fall after biosolids application could conserve some of this N and reduce the potential for leaching loss.
| ACKNOWLEDGMENTS |
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Received for publication December 13, 2002.
| REFERENCES |
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