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Published in Agron J 99:952-959 (2007)
DOI: 10.2134/agronj2006.0149
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Tillage

Corn and Soybean Production as Affected by Tillage Systems

Jeffrey A. Vetscha,*, Gyles W. Randalla and John A. Lambb

a Southern Research and Outreach Center, Univ. of Minnesota, 35838 120th St., Waseca, MN 56093-4521
b Dep. of Soil, Water and Climate, 1991 Upper Buford Cir., Univ. of Minnesota, Saint Paul, MN 55108

* Corresponding author (jvetsch{at}umn.edu)

Received for publication May 12, 2006.

    ABSTRACT
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 
Although continuous no-till (NT) cropping systems are appropriate on highly erodible land, concern among producers about potential yield reductions has limited NT adoption in the northern Corn Belt, especially on poorly drained soils. The objectives of this 4-yr study were to quantify the effects of rotational full-width tillage compared with long-term NT and zone-tillage (ZT) systems with and without in-season row cultivation (RC) on corn (Zea mays L.) and soybean [Glycine max (L.) Merr.] yield and economic return. The study was conducted on a tile-drained Nicollet–Webster clay loam soil complex. Sixteen of the 18 treatments comprised a factorial arrangement of three factors: (i) tillage for corn following soybean [NT, 38-cm deep fall ZT, 20-cm deep fall strip-tillage (ST), or spring field cultivate (SFC)], (ii) tillage for soybean following corn [NT or fall chisel plow (CP) plus SFC], and (iii) in-season RC for corn (with or without). Four-year average corn grain yields were greater for ST and ZT (10.1 Mg ha–1) compared with SFC (9.7 Mg ha–1) and NT (9.6 Mg ha–1) tillage for corn. No-tillage for the previous year's soybean crop reduced corn yields in two of 4 yr compared with full width (CP+SFC) tillage. Moreover, when full-width tillage for soybean was rotated with ZT or ST for corn, these treatments produced greater corn yields and economic returns than annual full-width tillage systems. Soybean yields were maximized by rotational tillage; however, the small differences in yields found among the tillage systems did not result in an economic return to full-width tillage practices. When both corn and soybean production was considered, rotational tillage practices were likely to maximize yields but not economic return.

Abbreviations: CP, chisel plow • GWC, gravimetric water content • NT, no-till • PR, penetrometer resistance • RC, row cultivation • SFC, spring field cultivate • ST, strip-tillage • ZT, zone-tillage


    INTRODUCTION
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 
NO-TILL CORN AND SOYBEAN PRODUCTION is appropriate on thousands of hectares of highly erodible land, but concern among producers about potential yield reductions has limited its adoption in the northern Corn Belt, especially on relatively flat, poorly drained soils. No-till adoption trends for Minnesota (1995–2000) have been steady to slowly declining (Conservation Technology Information Center, 2000). Adoption ranged from 6.6 to 4.3% for NT soybean production to <4% for NT corn. Hill (2001) categorized grower's use of NT practices throughout the northern Corn Belt and found that the lack of adoption has been linked to yield reductions in long-term NT. Short-term NT or rotational tillage systems may be advantageous in the northern Corn Belt because of time, labor, fuel savings, and conservation compliance.

The quantity of available literature on rotational tillage systems describing residue cover, yield, and economic return is not extensive. Some studies have focused on periodic full-width moldboard plow or CP tillage (Dickey et al., 1983; Randall et al., 1996); while others have evaluated deep ZT or subsoiling implements and their immediate and residual effects (Varsa et al., 1997; Soane et al., 1987; Marks and Soane, 1987; Vetsch and Randall, 2002). Generally, rotational tillage, either full-width (moldboard plow and CP) or deep ZT, has improved crop yields on moderately well to somewhat poorly drained soils (Dickey et al., 1983; Randall et al., 1996) and/or soils with dense layers (Varsa et al., 1997). Other researchers have found little to no effect of tillage on soils varying from poorly to well drained (Soane et al., 1987; Marks and Soane, 1987; Vetsch and Randall, 2002; Vepraskas et al., 1995). Randall et al. (1996) reported long-term NT reduced corn yields compared with conventional tillage, thus resulting in significantly greater risk to growers on poorly drained glacial till soils of south-central Minnesota. Yield reductions were magnified by unusual growing season climatic conditions (generally worse in wet and dry years). Vetsch and Randall (2002) found no corn yield response to semiannual, 38-cm-deep ZT in rotation with NT soybean on a silt loam in Minnesota.

No-till soybean production throughout the Corn Belt is more commonplace than NT corn production. The effects of tillage on soybean production are covered extensively in the literature. Yin and Al-Kaisi (2004) compared soybean yield in various tillage systems at five Iowa sites for periods ranging from 8 to 15 yr. At four of five sites (one site did not include CP tillage) NT soybean yields were not different compared with CP, when averaged across years. No-tillage reduced soybean yields compared with CP in one of 15 yr at the Nashua site and two of 6 yr at the Newell site. Significant differences between NT and CP were not found at the Crawfordsville site. When NT soybean yields were compared with other tillage systems over time (5-yr intervals), they found neither significant improvement nor deterioration of yield. They concluded NT soybean yields were usually within 5% of other tillage systems, but generally had equal or greater economic returns. Lueschen et al. (1992) found soybean yields were not affected by tillage on one of three glacial till sites in Minnesota, whereas significant yield differences were found in six of 11 site-years at two other sites. Yield differences among tillage treatments (moldboard, CP, spring disk, NT, ridge-till, and till-plant) at these two sites were small, ranging from 0 to 0.2 Mg ha–1 and were not consistent between sites. The authors concluded that the inconsistency in soybean yields among tillage systems makes it nearly impossible to single out any one tillage system as best for soybeans after corn. Randall et al. (1996) measured the effects of rotational tillage on soybean yields in a corn and soybean rotation. They found NT soybean yields in latter years of the study period were 0.3 to 0.4 Mg ha–1 less than when rotational full-width (CP and moldboard plow) tillage was used for corn. They suggested surface soil compaction and less-than-ideal weed control in some years may have led to these yield reductions. Randall et al. (2001) found soybean yields were not affected by tillage treatments [NT, one-pass (spring disk), and CP+SFC] on a low-P testing site in Minnesota, while on a high-P testing site NT yields were 0.1 to 0.2 Mg ha–1 less than the one-pass disk and CP+SFC tillage treatments. In Illinois on silt loam soils with claypans (southern locations) or dark–colored prairie soils (northern locations), Nafziger (2003) found soybean yields were not affected by deep tillage, although improvements in surface soil compaction and permeability were noted.

Many researchers have used soil penetrometer resistance (PR, cone index) to quantify benefits of periodic tillage in NT systems (Bauder et al., 1981; Busscher et al., 1986; Pierce et al., 1992; Vetsch and Randall, 2002). Bauder et al. (1981) showed long-term NT (10 yr) had greater PR than moldboard or CP on a clay loam soil. Busscher et al. (1986) found residual effects of subsoiling could be seen in the year following subsoiling on a coastal plain soil. However, PR in the year-old subsoil trench was considered to be root-limiting (1.5–2.5 MPa). They also noted that CP did not disturb the soil to the desired depth and took more energy than subsoiling. Pierce et al. (1992) found that PR approached 3.0 MPa in NT on a well-drained loam soil in Michigan but was reduced to 0.5 MPa by ZT and remained <1.0 MPa during the next 2 yr. Vetsch and Randall (2002) found in-row PR ranged from 0.2 to 1.1 MPa on a silt loam soil. Generally, ST (20-cm depth) and deep ZT (38-cm depth) reduced PR nearly to the depth of tillage compared with NT and one-pass, SFC (10-cm depth). However, PR between 45 and 60 cm was not different among treatments.

It is evident additional research is needed to better understand yield reductions in long-term NT and yield responses of corn and soybean to rotational tillage systems, especially on the highly productive but poorly drained soils of the northern Corn Belt. The primary objective of this study was to quantify the effects of rotational full-width tillage compared with long-term NT and ZT (20- and 38-cm-deep) systems with and without in-season RC on corn and soybean yield and economic return on a tile-drained clay loam soil in south-central Minnesota. A secondary objective was to characterize the effects of these tillage systems on residue coverage, early growth of corn, and soil PR.


    MATERIALS AND METHODS
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 
Field experiments were conducted from 2000 through 2004 at the University of Minnesota Southern Research and Outreach Center, Waseca, MN (44.06° N, 93.52° W) on a tile-drained Nicollet–Webster clay loam soil complex (fine-loamy, mixed, superactive, mesic Aquic Hapludolls and fine-loamy, mixed, superactive, mesic Typic Endoaquolls, respectively). The plots were planted perpendicular to subsurface tile drainage lines that were spaced 23 m apart. The 0.8-ha site consisted of two 0.4-ha units, which were rotated between NT corn and NT soybean from 1994 through 1999. Soil samples taken to a 15-cm depth in August of 1996 averaged 6.4 pH, 26 mg kg–1 Bray P1 (very high), and 176 mg kg–1 exchangeable K (very high), respectively (Rehm et al., 2001). Fertilizer P and K were broadcast applied at 73 and 186 kg ha–1, respectively, in October 2000 and at 50 and 140 kg ha–1 in October 2002.

Eighteen treatments were arranged in a randomized, complete-block design with four replications (blocks) for corn and an adjacent four replications for the soybean experiment. Sixteen of the 18 treatments comprised a factorial arrangement of three factors: tillage treatment for corn following soybean (NT, ZT, ST, and SFC), tillage treatment for soybean following corn (NT and CP+SFC), and in-season RC for corn (with or without). The other two treatments were annual CP+SFC treatments for both crops—one with RC for corn the other without RC. Each individual plot was 3 m wide (four 76-cm rows of corn) by 17.5 m long.

All corn plots, regardless of tillage treatment for corn, were planted with a John Deere (Moline, IL) Model 7300 planter equipped with Yetter (Colchester, IL) Residue Managers and a 36-cm-diam. ripple coulter mounted 5 cm to the side of the row. An injection nozzle located behind this coulter was used to inject a stream of liquid starter fertilizer to an 8-cm depth for all corn plots. Starter N and P were applied at 12 and 18 kg ha–1, respectively, in 2000, 2002, and 2003, and at 24 and 36 kg ha–1, respectively, in 2001. Corn [Pioneer hybrid 37H26 (37H27 in 2002)] was planted on 14 May 2001, 3 May 2002, and 29 Apr. 2003 at 79 000 seeds ha–1. Because a late spring frost on 17 May 2000 reduced stand, the study was replanted on 23 May 2000.

The NT treatment received no fall or preplant tillage before planting corn. The ZT treatment was deep zone-tilled to a 38-cm depth on 76-cm centers in the fall with a four-shank John Deere (Moline, IL) Model 955 Ripper (Vetsch and Randall, 2002). The ST treatment was performed to a 20-cm depth in the fall with a DMI (CASE DMI, Goodfield, IL) ST unit with mole knives (Randall and Hill, 2000). Corn was planted the following spring directly into the ST and ZT zones without preplant tillage. The SFC treatment was field cultivated to a 7- to 10-cm depth before planting. The CP+SFC treatment was chisel plowed to a 20-cm depth in the fall with a Hiniker (Mankato, MN) CP and field cultivated just before planting. In mid to late June, one-half of the treatments received RC to an 8-cm depth with a John Deere (Moline, IL) Model RM cultivator.

Nitrogen as urea with NBPT [N-(n-butyl)thiophosphoric triamide] was broadcast applied at 146 kg ha–1 on 9 May 2000. In 2001, 2002, and 2003, N was injected 10-cm deep between the rows as 28% UAN (urea–ammonium nitrate) at 146 kg N ha–1 as an early sidedress application. Weed control was performed with a combination of pre- and postemergence herbicide applications. Weed control was excellent in all years of the study.

Surface residue measurements were taken at a 45° angle to the rows after planting using the line-transect method described by Sloneker and Moldenhauer (1977). Extended-leaf plant heights were taken from 10 random plants {approx}35 d after emergence. Corn grain and soybean seed yield and moisture content were measured by harvesting two 17-m-long rows with a plot combine. Corn grain and soybean seed yields were expressed on a 15.5 and 13% moisture basis, respectively.

Soybean was planted in six 51-cm rows with a Hiniker (Mankato, MN) planter equipped with Dawn (Dawn Equipment, Sycamore, IL) row cleaners. The 51-cm row spacing of the planter resulted in soybean rows that were {approx}13 or 38 cm from the previous year's corn rows in the NT treatments. Soybeans (Pioneer 91B64) were seeded at {approx}325000 seeds ha–1. Inadequate stand establishment in 2002 required a replant on 30 May. In other years soybeans were planted on 1 May 2000 and 17 May 2001. The NT treatment received no fall or preplant tillage before planting soybean and the corn stalks were not chopped or shredded. The CP+SFC treatment was chisel plowed to a 20-cm depth in the fall with a Hiniker CP and field cultivated (8–10 cm deep) just before planting. Excellent weed control was obtained with postemergence applications of glyphosate herbicide.

Net economic return of corn and soybean production was calculated based on tillage cost estimates (Lazarus and Selley, 2005), corn and soybean yields from 2000 through 2002, and $29 and $73 Mg–1 prices (USDA "county loan rate") of corn and soybean, respectively. The gross income from corn and soybean production was summed for each plot before subtracting all of the tillage treatment costs for the corn–soybean rotation. The net return was then divided by two, assuming an equal proportion of corn and soybean in the crop rotation.

Penetrometer resistance was measured in 15-mm depth increments directly in the row area for all four tillage treatments with a Rimik CP10 recording penetrometer (Agridry-Rimik Pty. Ltd., Toowoomba, QLD, Australia) with a standard ASAE 30°, 12.8-mm cone. Three measurements from each main plot were taken in mid-April in 2000 (before spring tillage), mid-May in 2000 through 2002 (at emergence), and mid-June in 2000 [about V4 (Ritchie et al., 1986)]. At the same time and from the same area as PR measurements, soil samples (four cores per plot) were collected and analyzed for gravimetric water content (GWC) in increments of 0–10, 10–20, 20–30, and 30–45 cm. The in-row area in NT, SFC, and CP+SFC treatments was approximated for the April sampling. Statistical analysis and graphical display of PR data were simplified by combining the 15-mm PR measurements into a 75-mm increment and then averaging.

Daily precipitation and air temperature for the growing season were recorded at a weather station 0.3 km from the site. Analysis of variance statistics were performed using the GLM procedure of SAS (SAS Inst., 1999). All LSDs were calculated at P ≤ 0.05 for residue cover and crop production parameters and P ≤ 0.10 for soil GWC and PR.


    RESULTS AND DISCUSSION
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 
Growing season temperature and precipitation departures from normal are listed in Table 1. Generally, temperatures did not deviate much from long-term normals in any of the 4 yr of the study, except for cooler-than-normal temperatures in May 2002. Precipitation departures, both growing season and monthly, deviated markedly from long-term normals. Precipitation was 19 and 14% greater than normal in 2000 and 2001, respectively, and 31% less than normal in 2003. On a monthly basis, the growing seasons of 2000 through 2002 were characterized by months of significantly greater than and less than normal precipitation, while in 2003 precipitation was slightly to significantly less than normal in all months. It's unlikely that growing season temperatures had any significant effect on corn production. However, wetter-than-normal springs in 2000 and 2001 and drier-than-normal summer months in 2000 and 2003 may have affected corn production.


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Table 1. Growing season air temperatures and precipitation departures from normal for 2000–2003 at Waseca, MN.

 
Corn Grain Moisture
Corn grain moisture was affected by the main effects of year, tillage for corn, and tillage for soybean (Table 2). Grain moisture was 5 g kg–1 drier with CP+SFC tillage for soybean compared with NT for soybean, when averaged across year, tillage for corn, and RC. However, a significant year x tillage for corn interaction showed grain moisture was significantly drier when CP+SFC tillage was used for soybean compared with NT in 2000, 2002, and 2003, but not in 2001 (data not shown). Although grain moisture for the NT, ZT, ST, and SFC tillage systems for corn were significantly different when averaged across year, tillage for soybean, and RC, the differences were small and not agronomically significant.


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Table 2. Corn grain moisture, grain yield, soybean yield, and economic return to corn and soybean production as affected by tillage treatments.

 
Corn Grain Yield
Corn grain yield was affected by the main effects of year, tillage for corn, and tillage for soybean (Table 2). Corn grain yields, averaged across tillage systems, were significantly less in 2000 compared with other years because a late spring frost reduced stand and required replanting on 23 May and drier-than-normal conditions in August and September. Zone-till and ST for corn increased yields 0.4 to 0.5 Mg ha–1 (6 to 7 bu ac–1) compared with SFC and NT, respectively, when averaged across year, tillage for soybean, and RC. An annual CP+SFC treatment (conventional tillage for corn and tillage for soybean) averaged 10.1 Mg ha–1 which was equal to ZT and ST for corn (data not shown). No-tillage for the previous year's soybean crop reduced yields 0.4 Mg ha–1 (6 bu ac–1) compared with CP+SFC tillage, when averaged across year, tillage for corn, and RC. However, a significant year x tillage for soybean interaction showed NT for soybean decreased grain yields 0.3 and 1.0 Mg ha–1 compared with CP+SFC in 2000 and 2002, respectively, but had no effect on yields in 2001 and 2003 (Table 3). Similar to Randall et al. (1996), these data show that reduced yields with long-term NT systems compared with rotational tillage systems did not occur every year. However, in some years yield reductions can be large. They found rotational tillage systems increased corn yields compared with long-term NT systems during unusual growing seasons (droughty or cool and wet). An evaluation of the yield response for rotational tillage in this study found no consistent relationship with monthly or growing season temperature or precipitation.


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Table 3. Corn grain yield as affected by an interaction between year and tillage for soybean, when averaged across tillage for corn and row cultivation.

 
The significant year x RC x tillage for soybean interaction showed RC increased corn yield 0.2 and 0.6 Mg ha–1 in 2000 and 2002, respectively, when NT was used for soybean; whereas when CP+SFC tillage was used for soybean, RC decreased corn yield 0.2 and 0.6 Mg ha–1 in 2000 and 2002, respectively (data not shown). This interaction was not related to RC enhancing weed control, as weed control was excellent in all years. Moreover, this interaction showed yields were increased with either shallow RC for corn or deep rotational full-width tillage for soybean in two of 4 yr. This significant interaction suggests the reasons for periodic yield responses with rotational full-width tillage may be caused by a combination of factors, such as reduced residue cover, warmer soils, more favorable soil moisture, and less surface soil compaction.

Soybean Seed Yield
Soybean seed yield was affected by the main effects of year and tillage for soybean, but not by tillage or RC for corn (Table 2). Soybean yields were 0.07 Mg ha–1 (1 bu ac–1) greater with CP+SFC tillage for soybean compared with NT when averaged across years, tillage for corn, and RC for corn. This small yield difference was similar to those found by Lueschen et al. (1992).

Several significant interactions were found for soybean yield including: year x tillage for soybean, tillage for corn x tillage for soybean, RC x tillage for soybean, and tillage for corn x RC (Table 2). These findings may help explain soybean yield responses in reduced and rotational tillage systems on poorly drained clay loam soils. The year x tillage for soybean interaction indicated the yield effects of tillage for soybean varied among years (data not shown). Soybean yields with NT were 0.24 Mg ha–1 less than CP+SFC tillage in 2000, but not significantly different in 2001 and 2002. Reduced yields with NT in 2000 may have been related to a wetter-than-normal spring. The tillage for corn x tillage for soybean interaction (data not shown) is explained by soybean yields being increased 0.12 Mg ha–1 or more when CP+SFC tillage was used for soybean compared with NT in NT and ZT systems for corn, but not in SFC or ST systems for corn. When CP+SFC tillage for soybean followed ZT for corn, soybean yield was greater than any other treatment combination, suggesting a yield benefit for rotational full-width tillage. However, the yield response obtained with CP+SFC tillage was negated when RC was used for the previous corn crop. Under these conditions periodic shallow tillage, like RC for a previous corn crop, was apparently adequate to disrupt residue accumulation and soil consolidation and enhance soybean growth. This treatment combination (NT for soybean following corn that received RC) had yields similar to CP+SFC tillage for soybean, while maintaining about 78% residue cover (data not shown). The tillage for corn x RC interaction resulted from a soybean yield response when RC was coupled with NT for corn, but no response when RC for corn was used with other tillage systems for corn (data not shown). These data show that some form of rotational tillage, however minimal for surface soil disturbance, was needed to maximize soybean yield.

The yield responses to surface soil disturbance found in this study may be related to the placement of the soybean rows with respect to the previous year's corn rows. The 51-cm row spacing of the soybean planter resulted in four soybean rows that were {approx}13 cm from a previous year's corn row and two soybean rows that were {approx}38 cm or midway between the previous year's corn rows in the NT for soybean treatments. Moreover, when NT was used for soybean, these two 38-cm rows were seeded directly into wheel traffic areas from the previous year's corn crop. Slightly slower emergence and early growth were observed in these rows, especially following NT for corn without RC, indicating a less-than-ideal seed bed under these undisturbed conditions. However, these findings are not unique to the row spacing used in this study. Any corn–soybean rotation, where the row spacing for soybean is less than used for corn, would experience NT soybean rows planted into wheel-tracked areas from the previous crop.

Economic Return to Tillage Costs
Economic return for the combined corn–soybean rotation was affected by the main effects of year and RC (Table 2). Economic return, averaged across tillage treatments, was significantly greater in 2002 compared with other years because of greater corn yields. Row cultivation of corn reduced economic return $7 ha–1 compared with no RC, when averaged across year, tillage for corn, and tillage for soybean. The small corn and soybean yield responses to tillage for soybean and corn yield response to tillage for corn found in this study did not affect the economic return of those main effects in this study.

Significant interactions were found for year x tillage for soybean, year x tillage for corn x tillage for soybean, and RC x tillage for soybean. The year x tillage for soybean interaction showed CP+SFC tillage for soybean increased economic return in 2000 and 2002, but reduced economic return in 2001 (data not shown). These data parallel the differences found with corn yield, which suggests CP+SFC tillage for soybean had a greater effect on corn yield than it did on soybean yield. The significant year x tillage for corn x tillage for soybean interaction (data not shown) was similar to the year x tillage for soybean interaction. In 2001, NT for soybean had greater economic return than CP+SFC tillage for soybean for all tillage for corn systems, whereas in 2000 and 2002 CP+SFC tillage for soybean had significantly greater return than NT for soybean but only when ZT or ST was used for corn. Moreover, in 2000 and 2002, greatest economic returns were obtained when ZT or ST was used for corn with CP+SFC tillage for soybean (data not shown). The RC x tillage for soybean interaction was illustrated by RC of the previous year's corn, increasing economic return $9 ha–1 when NT was used for soybean, whereas RC of corn reduced soybean return $23 ha–1 when CP+SFC tillage was used for soybean (data not shown). In summary, rotational tillage practices are likely to maximize yields of corn and soybean but not consistently increase economic return on these clay loam soils.

Surface Residue Cover after Planting Corn
Residue cover measured after planting was affected by all of the main effects (Table 4). Residue cover was 67, 41, 56, and 41% with NT, ZT, ST, and SFC tillage for corn, respectively, when averaged across year, tillage for soybean, and RC. No-tillage for the previous year's soybean crop resulted in an 11 percentage point greater residue cover for corn compared with CP+SFC tillage when averaged across year, tillage for corn, and RC. These percentage residue covers are typical for continuous reduced tillage systems in a corn–soybean rotation in the Northern U.S. latitudes due to slow decomposition. Residue from both the previous soybean crop as well as the prior corn crop is plentiful in the spring.


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Table 4. Residue cover after planting corn and soybean and corn plant height as affected by tillage treatments.

 
The tillage for corn x tillage for soybean interaction showed a 14 to 15 percentage point reduction in residue cover when CP+SFC tillage was used for soybean compared with NT soybean, except for the ZT system for corn where residue cover was reduced only three percentage points (data not shown). Generally, CP+SFC tillage for soybean helped keep residue cover at more manageable levels compared with NT for soybean in rotation with reduced tillage for corn. The year x tillage for corn interaction showed residue cover with ST for corn was 20 and 17 percentage points less than NT in 2000 and 2003, respectively, whereas differences in residue cover found between ST and NT in 2001 and 2002 were not significant (data not shown). These data indicate residue coverage in ST can be similar to NT in years where overall residue levels are less.

Residue Cover after Planting Soybean
Residue cover, measured after planting soybean, was affected by the main effects of year and tillage for soybean but not by the residual effects of tillage or in-season RC of corn (Table 4). No-tillage for soybean had significantly greater residue cover (79%) compared with CP+SFC (33%). No significant interactions were found. Residue cover in all treatments (data not shown) was greater than the 30% threshold recommended for minimizing soil erosion, when averaged across the 3-yr study period.

Corn Plant Height
Early growth of corn, often measured in terms of plant height, is frequently used by farmers and ag advisors to evaluate the relative performance of conservation tillage systems. Plant height {approx}35 d after emergence was affected by all of the main effects (Table 4). When NT was used for soybean compared with CP+SFC tillage, plant heights were reduced considerably, when averaged across year, tillage for corn, and RC. Plant heights were affected by tillage for corn and were ranked ZT > ST > SFC = NT, when averaged across year, tillage for soybean, and RC. Zone tillage increased plant heights 4% compared with ST, but had no affect on corn yields. Row cultivation of corn decreased plant height although the difference was small and inconsequential. Significant interactions were found for tillage for corn x tillage for soybean, RC x tillage for soybean, and year x tillage for corn. The tillage for corn x tillage for soybean interaction showed plant heights responded more to CP+SFC tillage for the previous year's soybean in SFC and NT for corn compared with ZT and ST for corn (data not shown). These data demonstrate the beneficial effects of in-row tillage and residue removal in the seed–row zone with ST and ZT for greater early growth of corn. The RC x tillage for soybean interaction had no plausible explanation (data not shown).

Soil Gravimetric Water Content
Tillage treatments affected GWC (data not shown) in only five of 48 sampling time/depth increment comparisons: April (0–10 cm) and June (11–20 cm) of 2000, 2001 (0–10 and 31–45 cm), and 2002 (11–20 cm). However, differences were relatively small among tillage treatments within a sampling time/depth increment. Gravimetric water content ranged from 0.255 to 0.281, 0.242 to 0.279, 0.267 to 0.288, 0.227 to 0.250, and 0.274 to 0.297 g g–1 in April (2000), June (2000), 2001 (0–10 cm), 2001 (31–45 cm), and 2002 (11–20 cm), respectively. A factorial analysis of the GWC data from 2000 (tillage for corn x tillage for soybean) showed GWC was not affected by tillage for soybean during any of the sampling times or depths. Variation in soil water content can influence or mask differences in PR. However, it's unlikely the small differences in GWC data influenced the PR measurements in this study.

Penetrometer Resistance
In April (preplant), May (corn emergence), and June (about V4) of 2000, in-row PR measurements were taken to evaluate the immediate and residual effects of fall and spring tillage for corn (Fig. 1 ). Penetrometer resistance ranged from 0.25 to 1.43 MPa across sampling dates and tillage treatments. No-till and SFC treatments had similar PR throughout the 60-cm profile in all 3 mo. In April, PR was reduced to a 30-cm depth by ZT and ST and to a 15-cm depth by CP+SFC for corn, compared with NT and SFC. By May, some reconsolidation had occurred in ZT, ST, and CP+SFC for corn, but PR in these treatments was less than NT and SFC at similar depths as in April. In June, PR was reduced by ZT and ST in the 8- to 30- and 8- to 22-cm increments, respectively, compared with NT, SFC, and CP+SFC. Differences among treatments in the 0- to 8-cm increment were small. Like Pierce et al. (1992) and Vetsch and Randall (2002), in-row PR was reduced considerably down to the effective depth of tillage with ZT and ST, but some reconsolidation occurred in May and June. Similar to Dickey et al. (1983), Diaz-Zorita et al. (2004), and Vetsch and Randall (2002), PR never exceeded threshold values where root restrictions would be expected. A factorial analysis of these data found CP+SFC tillage for the previous year's soybean crop reduced PR in the 0- to 15-cm increment compared with NT in April, but not in May or June (data not shown). A significant tillage for corn x tillage for soybean interaction was explained by PR in the NT and SFC systems for corn being less when the previous crop of soybean was CP+SFC compared with NT, but tillage for soybean had no effect on PR with ZT and ST. The immediate effects of tillage for corn on in-row PR were evident at the April and May sampling times for ZT, ST, and CP+SFC, while the residual effects of fall ZT and ST systems for corn were still evident in June.


Figure 1
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Fig. 1. In-row penetrometer resistance in April (before preplant tillage), May (corn emergence), and June (about V4) in 2000 as affected by tillage for corn. Error bars at each depth show LSD (0.10). CP+SFC, chisel plow plus spring field cultivate (SFC); ST, strip-tillage; ZT, zone-tillage; NT, no-tillage.

 
Differences in growing seasons and climatic conditions were evaluated by comparing PR in May across the 3-yr period (Fig. 2 ). Penetrometer resistance ranged from 0.29 to 1.23, 0.32 to 1.03, and 0.23 to 1.29 MPa for 2000, 2001, and 2002, respectively. Tillage treatments affected in-row PR to a 38-, 60-, and 38-cm depth in 2000, 2001, and 2002, respectively. Tillage treatment effects on PR in 2000 were discussed earlier. In 2001 PR responses to tillage treatments were similar to 2000, however, the magnitude of the PR values was less than in other years (generally <1.00 MPa) especially for the NT, SFC, and CP+SFC treatments. Significant differences in the 38- to 60-cm depth in 2001, not seen in other years, were small. Generally, ST, SFC, and ZT reduced PR more than the NT and CP+SFC treatments. The largest difference in PR among tillage systems occurred in 2002, where ZT averaged 0.38 MPa between 15 and 38 cm compared with the other treatments, which averaged 1.16 MPa. This large difference could be related to greater fracturing (loosening) of the soil by ZT in the fall of 2001 or less reconsolidation of ZT during the spring planting season of 2002. During the 3-yr period, PR never exceeded threshold values where root restrictions would be expected (Unger and Kaspar, 1994). Moreover, PR did not increase in NT or shallow tillage (SFC) systems as reported by Bauder et al. (1981).


Figure 2
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Fig. 2. In-row penetrometer resistance in May (corn emergence), from 2000–2002 as affected by tillage for corn. Error bars at each depth show LSD (0.10). CP+SFC, chisel plow plus spring field cultivate (SFC); ST, strip-tillage; ZT, zone-tillage; NT, no-tillage.

 

    CONCLUSIONS
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 
Tillage system research conducted on a tile-drained clay loam soil for corn and soybean production in south-central Minnesota showed (i) corn grain yields were greater with ZT and ST for corn than NT and SFC, and in 2 of 4 yr, corn yields were greater when CP+SFC tillage was used for the previous year's soybean crop compared with NT for soybean; (ii) soybean seed yields were increased in only 1 of 3 yr [0.07 Mg ha–1 (1 bu ac–1) when averaged across years] by CP+SFC tillage for soybean compared with NT for soybean; (iii) the small corn and soybean yield responses to tillage did not improve the economic return in this corn–soybean rotation; and (iv) significant reductions in PR at the 15- to 38-cm soil depth from deep ZT did not increase economic return. The many significant interactions found among the main effects for corn and soybean yields and economic return showed some form of rotational tillage (i.e., CP+SFC tillage for soybean or RC of corn) was likely to increase yields for one if not both crops, but was less likely to effect economic return. Thus, the primary benefit of rotational tillage practices may be in reducing risk of yield loss in some years and managing residue accumulation but not necessarily increasing economic return over less aggressive tillage systems on these relatively flat clay loam soils.


    ACKNOWLEDGMENTS
 
The authors thank David Groh for his assistance in collecting the data. Partial funding provided by John Deere Co. for this research was greatly appreciated by the authors.


    REFERENCES
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS AND DISCUSSION
 CONCLUSIONS
 REFERENCES
 




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