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a Univ. of Florida, IFAS, Agronomy Dep., 304 Newell Hall, Gainesville, FL 32611
b Univ. of Florida, IFAS, Agricultural and Biological Engineering Dep., 120 Frazier Rogers Hall, Gainesville, FL 32611
* Corresponding author (jmscholberg{at}ifas.ufl.edu)
Received for publication July 26, 2006.
| ABSTRACT |
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Abbreviations: DAT, days after transplanting ETc, actual crop evapotranspiration SE, standard error VWC, volumetric water content
| INTRODUCTION |
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Under conditions that prevail in the southeastern USA, most soil N is rapidly converted to nitrate N (Jansson and Persson, 1982). Nitrate moves with the wetting front and N leaching on sandy soils is intrinsically linked with soil water dynamics. Actual N leaching losses depend on N source and application rates, crop removal capacity, and water displacement below the active root zone. Excessive irrigation and/or N application rate combined with intense rainfall on excessively drained sandy soils with low water-holding capacity greatly enhances the potential risk of N leaching (Knox and Moody, 1991; McNeal et al., 1995). Nitrate leaching from agricultural fields is considered to be one of the major contributors to groundwater contamination and 25% of surficial groundwater samples collected from agricultural areas of the Georgia-Florida coastal plain exceeded the USEPA nitrate standard for drinking water of 10 mg NO3N L1 (USGS, 1998).
For vegetable crops, the introduction of plastic mulch, drip irrigation, and recently subsurface drip irrigation (Thompson et al., 2002; Lamm and Trooien, 2003) reduced soil water evaporation and potential nitrate leaching (Romic et al., 2003). The use of drip irrigation also facilitated fertilizer injection to irrigation systems (fertigation), which improved the synchronization between nutrient application and crop nutrient uptake (Bowen and Frey, 2002). On sandy soils, fertigation combined with plastic mulch may reduce nutrient leaching (Romic et al., 2003; Vázquez et al., 2006). Improved irrigation management will be a key requirement for enhancing fertilizer use efficiency which is critical for reducing nitrate loading of groundwater resources. A key criterion for assessing the effectiveness of best management practices (BMPs) to enhance water quality will be their effectiveness in reducing nitrate leaching.
Different methods have been employed to assess N leaching in unsaturated soils (Barbee and Brown, 1986; Lord and Shepherd, 1993; Webster et al., 1993; Pampolino et al., 2000). Soil coring is simple, relatively cheap, widely used, and applicable to most soils. However, soil coring can be time-consuming, it is destructive, and it only provides a "snapshot" of N distribution. In comparison with other methods, soil sampling provides an indirect measurement of inorganic N in the soil solution (Webster et al., 1993). Repeated soil coring may also introduce errors associated with inherent spatial variability in soil nitrate concentration, which may be an issue for drip-irrigated vegetable systems on coarse sandy soils that may have fairly pronounced lateral water and nutrient gradients (Simonne et al., 2004b). Although soil coring will provide information on N distribution within the soil profile and N balances at a single point in time, this method is not suitable to calculate N leaching unless it is combined with modeling approaches and/or by linking soil N distribution with water flow dynamics below the rhizosphere (Willian and Nielsen, 1989).
Ceramic suction cup lysimeters are considered to be a suitable technique to monitor N leaching in non-structured soils (Webster et al., 1993). They are easy to install and allow repeated measurements from the exact same location, but they do not allow development of mass balances at a single point in time unless potential soil water flux is determined at the same time. Moreover, under low soil water availability and dry conditions that often prevail in coarse sandy soils, it is often not possible to obtain adequate sample volumes, which may induce large uncertainties in calculating N losses (Barbee and Brown, 1986; Lord and Shepherd, 1993).
Drainage lysimeters are commonly used to monitor N leaching dynamics. They capture the entire leachate volume and N concentration, which can then be used to calculate N load passing below a specific soil depth. However, installation may result in appreciable soil disturbance. Also, they must be sized to represent a production unit. Finally, lysimeters need to be placed deep enough so that soil water conditions in the crop root zone represent overall field conditions, yet shallow enough to ensure adequate drainage and to ensure that time trends match actual N displacement below the effective root zone. Similar to the use of ceramic suction cups, the use of drainage lysimeters allows for direct and relatively consistent and precise measurement of nitrate concentrations (Webster et al., 1993). An additional advantage of this method is that it provides an "integrative approach" (both in space and time) which may be a more realistic way of assessing total N loads compared with other approaches that represent a relatively small spatial dimension (<5 cm) and only provide a "snapshot" of N leaching patterns.
The objective of this study was to compare the effectiveness of three different methods for monitoring and quantifying N leaching below mulched vegetable production beds as affected by the volume of irrigation and N rate.
We hypothesized that the use of different methods to monitor N leaching will result in similar estimates of overall cumulative N leaching rates independent of the volume of irrigation or N rate applied.
| MATERIALS AND METHODS |
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Two weeks before vegetable transplanting, raised beds of approximately 32-cm height were constructed. Beds were fumigated (80% methyl bromide, 20% chloropicrin by weight) at a rate of 604 kg ha1 concomitant to placement of both drip tape and plastic mulch in a single pass. Raised beds were 15 m long and 0.9 m wide with the bed centers spaced 1.8 m apart.
Vegetable crops grown were pepper (Capsicum annuum L., Brigadier), tomato (Lycopersicon esculentum Mill., Florida 47), and zucchini (Cucurbita pepo L. Wild Cat). Tomato and bell pepper were transplanted on 7 Apr. 2005. Peppers were planted in staggered twin rows at 0.3-m spacing both between and within the row. Tomato was planted in a single row at 0.45-m plant spacing. Zucchini seed was sown on 26 Sept. 2005 in a single row per plot, with 0.45-m spacing between plants.
The experiment compared the nitrate leaching for different irrigation rates and three methods of measuring nitrate leaching. The experimental design consisted of factorial irrigation rates (two for tomato and zucchini and three irrigation rates for pepper) assigned at random to the whole plots within each block. The methods were assigned to the subplots within each whole plot. The plot design was a randomized complete block design with four replicates (blocks).
Fertilizer was applied as weekly fertigation schedules based on IFAS (Institute of Food and Agricultural ScienceUniversity of Florida) recommendations (Maynard et al., 2003a, 2003b, 2003c). Nitrogen fertilizer application rates corresponded with either 100% (1.0 IFAS) or 150% (1.5 IFAS) of the recommendation for each crop. Weekly fertigation rates and cumulative amount of N applied are outlined in Fig. 1 and Table 1. The leaching potential of sandy soils is very high (McNeal et al., 1995). To reduce N leaching, N application rates were relatively low during initial growth, greatest during the linear growth phase, and gradually reduced toward the end of the growing season (Fig. 1). For pepper and tomato, N application rates were 11.7 kg N ha1 wk1 (wk 12) and 15.6 kg N ha1 wk1 (wk 34). Rates increased during the linear growth phase to 19.6 kg N ha1 wk1 (wk 511) before being reduced to 15.6 kg N ha1 toward the end of the growing season. For zucchini, application rates of 11.7 kg N ha1 wk1 (wk 12) were increased to 19.6 kg N ha1 wk1 (wk 37) before being reduced to 11.7 kg N ha1 wk1 (wk 89) before final harvesting (Fig. 1). All other nutrients were applied at recommended rates. All phosphorus (112 kg P2O5 ha1) and micronutrients were applied before applying plastic mulch to beds.
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Irrigation
Irrigation was applied via drip tape (Turbulent Twin Wall, 0.2-m emitter spacing, 0.25-mm thickness, 3.8 L h1 at 69 kPa, Chapin Watermatics, Watertown, NY). Two drip tapes were used, one for irrigation and one for fertigation. Irrigation treatments consisted of three different management and/or scheduling approaches; two sensor-controlled, and one fixed-time irrigation, resulting in different volumes of water applied to the crops. Two control sensors were used, a University of Florida designed quantified irrigation controller (QIC) system (Muñoz-Carpena et al., 2007) that allowed time-based irrigation (five potential irrigation events per day) if soil volumetric water content (VWC) dropped below a threshold value previously established. The commercially available Acclima RS500 soil moisture sensor (Median, ID) with a VWC threshold value that allowed time-based irrigation events similar to QIC was also used for selected treatments. The third irrigation approach, included as a control treatment, was a fixed time irrigation schedule (grower practice) in which water was applied 1 or 2 h per day depending on crop growth stage.
Water applied by irrigation or by fertigation was recorded by positive displacement flow meters (V100 1.6-cm diam. bore with pulse output, AMCO Water Metering Systems, Inc., Ocala, FL). Weekly manual meter measurements were taken and data from transducers that signaled a switch closure every 18.9 L were collected continuously by data loggers on each meter (HOBO event logger, Onset Computer Corp., Inc., Bourne, MA). Pressure was regulated by inline pressure regulators to maintain operating pressures of 83 kPa at the irrigation source and an average pressure in the field of 69 kPa during irrigation events.
Monitoring Nitrogen Methods
For monitoring N the following methods were evaluated: (i) soil coring at 0.3-m increments to a soil depth of 0.9 m; (ii) use of ceramic suction cups placed vertically in the center of the plots 0.9 m below the drip tape; and (iii) subsurface drainage lysimeters installed 0.75 m beneath the top of the beds. Samples were collected in each block for all methods. Ceramic suction cups and drainage lysimeters were placed next to each other and the soil samples were taken adjacent to other devices. Each collection method was replicated four times in corresponding field plots for each treatment.
Soil samples were collected biweekly using a 50-mm diam. soil auger. Samples were obtained 6 d after the previous fertigation and 1 d before the next one. A 10-g subsample was extracted with 50 mL of 2 M KCl and filtered by gravity (Q8, Fisher Scientific Inc., Pittsburgh, PA) within 1 d of soil sampling (Mulvaney, 1996). The gravimetric water content was determined for each depth interval and was used (by multiplying by the bulk density) to give the VWC.
Ceramic suction cups with an outside diameter of 48 mm and a height of 51 mm (Soilmoisture Equipment Corp., Santa Barbara, CA) were connected to a 1.0 m long PVC pipe closed at the top with a two-hole rubber stopper. Soil solution samples were collected weekly by applying approximately 70 kPa vacuum to the cups 6 d after the previous fertigation and 1 d before the next one. Samples were collected 24 h after the vacuum was applied just before the next fertigation.
Subsurface drainage lysimeters were installed in September 2004 in such a manner that they collected leachate for a representative transect of the production bed. The 0.75-m installation depth was selected since it was shallow enough to facilitate burial and sampling yet was below the effective root zone of tomato (Oliveira et al., 1996, Machado et al., 2003), pepper, and zucchini. Lysimeters were constructed out of 208-L capacity drums that were cut in half lengthwise. They were 0.85 m long, 0.27 m high, and had a diameter of 0.55 m. A 0.80 m long slotted pipe (well screen, slot size = 0.3 mm) with a diameter of 32 mm was capped at both ends and placed in the bottom of each lysimeter. One end of the slotted pipe was fitted with a 6.4-mm i.d. butyl rubber suction tube (Fisher Scientific Inc., Pittsburgh, PA) that was routed to the bottom of the raised bed to allow extraction of the leachate collected at the bottom of the lysimeter by a vacuum pump. The leachate was removed weekly, a day before the next fertigation by applying a partial vacuum (3540 kPa) using 20-L high vacuum bottles (Nalge Nunc International, Rochester, NY) placed in the vacuum line for each drainage lysimeter (Fig. 2 ). Leachate volume was determined gravimetrically and subsamples were collected from each bottle for NO3N analysis. Samples were extracted on weekly intervals as more frequent extraction would result in erratic sampling results and biweekly sampling would increase the excessive water accumulation, increasing the potential for denitrification.
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Statistical Analysis
Statistical analyses were performed using Proc GLM of SAS (SAS Institute, Inc., 1996) to evaluate the capacity of each method for each cropping system. Means were compared using Duncan's Multiple Range test (P < 0.05). PROC GLM was used to correlate overall seasonal N leaching for the N monitoring methods across cropping systems, irrigation treatments, and N rates.
Since irrigation and fertigation patterns affect N leaching, assessment of the effectiveness of different methods to monitor N leaching requires a basic understanding of leaching dynamics. Therefore, drainage and N leaching dynamics for the three systems as affected by irrigation and N management practices are outlined before comparing and discussing the performance of N leaching assessment methods.
| RESULTS AND DISCUSSION |
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In contrast to the low irrigation volume treatments, measured leachate for the greater volume treatments increased throughout the growing season (Fig. 3). The irrigation volume applied to P2 and T2 treatments was 170 to 329 mm, respectively, resulting in 29 and 43 mm of leaching below the effective root zone, which translated to about 18% of total irrigation water. In P3 and Z2, the leaching fraction was much higher and respective values were 60 and 67 mm. Applying irrigation below ETc (P1 and T1) resulted in a reduction of more than 50% of the leachate volume (Fig. 3). Irrigation rates for P3, Z1, and Z2 treatments, on the other hand, typically exceeded ETc (by 60%) throughout the entire growth period, resulting in a continuous increase in cumulative leaching. In contrast, weekly increments in drainage volumes decreased significantly for P1, P2, and T1 treatments after initial crop establishment (Fig. 3) because of higher plant ETc and lower rates of irrigation applied to these treatments.
Nitrogen Leaching Dynamics
The volume of irrigation had a significant effect on N leaching for all cropping systems (Table 2), except for zucchini due to the higher volume of irrigation applied compared with pepper and tomato crops. Because of weekly fertigation with calcium nitrate, solubilization, nitrification, soil N retention, and volatilization did not affect nor delay N leaching patterns, so they were directly linked to fertigation events. Due to the very low soil organic matter content of the top soil (<6.8 g C kg1) and the 60- to 90-cm soil layer (<2 g C kg1), N mineralization/immobilization was too low to affect leaching results either.
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In general, nitrate leaching followed similar trends as overall drainage (Fig. 3). However, the application of N rates above IFAS recommendations increased N leaching by 66% (19 vs. 32 kg N ha1), 63% (12 vs. 19 kg N ha1), and 32% (17 vs. 22 kg N ha1) for pepper, tomato, and zucchini, respectively. For pepper, nitrate leaching was also significantly lower for the P1 treatments (low volume of water applied) compared with all other irrigation treatments. With the use of high irrigation rates (e.g., P3 and T2 treatments), on the other hand, N leaching increased with N rate (Table 2).
Comparison between Methods of Nitrate Leaching Measurements
Multiplying net drainage volumes obtained from drainage lysimeters by nitrate solution concentration values below the effective root zone (60 cm) via soil coring and/or ceramic cups allowed us to calculate N loading rates for these methods as well. Nitrate leaching for all three methods were calculated as a function of cumulative drainage depth for each irrigation treatment.
In most cases there was a significant effect of volume of irrigation on the total amount of N that was being leached. Applying fertilizer in excess of IFAS recommendations tended to greatly increase N loss. For all crops there were discrepancies in measured concentrations between methods. Considering overall nitrate loads (kg NO3N ha1) regardless of irrigation treatments or nitrogen rate, ceramic suction cups had significantly lower nitrate load means compared with the drainage lysimeter and soil core methods for pepper and zucchini (Table 2; Fig. 4 , 5 , and 6 ). For tomato these effects were only significant for the T3 irrigation treatment.
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On the other hand, for treatments that received greater irrigation volume, such as T2 and Z1 and Z2, N loads measured by ceramic suction cups were typically lower than those based on drainage lysimeter measurements (Table 2; Fig. 5 and 6). Overall nitrate concentrations from ceramic suction cups were slightly lower than the nitrate concentration measured in the drainage lysimeters. Similar results were reported by Webster et al. (1993). Barbee and Brown (1986) proposed that ceramic suction cups were not suitable for monitoring water percolation through the soil profile under excessively wet conditions and/or for soils with high hydraulic conductivities.
When comparing soil cores and drainage lysimeter results for tomato (T2) and zucchini (Z2) with the 1.5 IFAS N rate, the opposite trend occurred. Soil core- and suction cup-based measures were relatively low compared with drainage lysimeters. This result may be related to N displacement below the sampling depth. Similar trends were observed by Barbee and Brown (1986) and Lord and Shepherd (1993). Soil extraction procedures can also affect nitrogen concentration and may impact solubility and calculation of solution concentrations. However, in our case the soil was a relatively inert medium. Due to the very low percentage organic matter (OM%) and cation exchange capacity (CEC) values of sandy soils and in the absence of NH4, these interferences in our system were minimized.
To make an overall assessment of the different methods across time and production systems sample, sets were integrated into a single data set. There was a close correlation (r2 = 0.86) between use of soil cores and drainage lysimeter (Fig. 7A ). However, for the low N range, calculated N loading rates based on soil coring were slightly higher compared with those based on drainage lysimeters (Fig. 7A). However, at higher N loading values the reverse was true; soil coring-based values were 28% lower compared with drainage lysimeter-based estimates. There was also a close correlation (r2 = 0.86) between ceramic suction cup lysimeter-based N loading estimates and those based on drainage lysimeters (Fig. 7B). However, in this case N loading values based on suction cup lysimeters were up to 42% lower compared with those derived from subsurface drainage lysimeters. Although ceramic suction cup lysimeter- and soil core-based N loading estimates were closely correlated (r2 = 0.67), suction cup lysimeter-based N loading estimates were up to 28% lower compared with soil coring-based estimates (Fig. 7C).
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With the use of subsurface drainage lysimeters, all of the N that was displaced below the effective root zone was retained since it accumulated at the bottom of the barrel. In this case, employing a partial vacuum allowed us to extract the entire intercepted leachate volume associated with a 0.84 m wide section of the production beds within 6 d after a specific fertigation event. With the use of ceramic suction cup lysimeter and soil core methods, sampling appeared to be more of a "snapshot" approach at biweekly intervals. Some of the nitrate leaching through the soil profile may have passed below the sampling point between sampling events. In this case, weekly sampling may be required to capture the complete N spike before it is displaced below the suction cup. On the other hand, according to Lord and Shepherd (1993), high sampling frequency is not recommended (shorter than bi-weekly) for suction cup lysimeters, since the applied vacuum may affect overall solution flow and/or drainage (Van der Ploeg and Beese, 1977).
In the case of the drainage lysimeters, we used weekly sampling and the drainage was typically less than 5 mm wk1. Although we also used a partial vacuum to pump the drainage lysimeters, this vacuum was not applied via a porous cup and therefore soil tension within the drainage lysimeter was limited to the air entry value of the soil (<40 kPa) and was not assumed to affect water flow within the effective root zone.
Although the drainage lysimeters were used as a reference method to measure the volume drainage and N loads, some factors may still interfere with nitrate measurements even with this approach. Accumulation of water in the bottom of the drainage lysimeters between sampling dates may enhance denitrification loss that would result in an underestimation of potential N leaching. However, in the absence of anaerobic conditions (which we verified in a follow-up study), denitrification rates for sandy soils in Florida are typically low due to the low soil carbon content (Espinoza, 1997). The use of weekly samplings combined with a partial vacuum allowed for an effective extraction of leachate at the bottom of the drainage lysimeter and the absence of anaerobic conditions. After sampling, soil water in the bottom of the barrel dropped to 15 to 20% VWC and the soil system remained oxygenated between samplings, thereby minimizing denitrification potential.
A second point of concern is roots reaching the bottom of the lysimeter and taking up nitrate accumulating there that would otherwise have bypassed the root system. However, root growth studies have shown that the majority of the root system is concentrated in the upper 0.25 to 0.3 m of the production bed (Goyal et al., 1988). Since the drainage lysimeters were installed at 0.75-m soil depth, root concentrations in the bottom of the drainage lysimeter, even at the end of the growing season, would have been minute (<5% of total root length), and should not significantly interfere with the N leaching assessment (Zotarelli et al., unpublished data, 2006).
| CONCLUSIONS |
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| ACKNOWLEDGMENTS |
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| REFERENCES |
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