Soil erosion is a problem in the Southeastern Coastal Plain of the U.S.A. where clean tillage row cropping exists without adequate soil conserving practices. Conservation tillage practices in the region have frequently incorporated in-row subsoiling to overcome root restricting soil layers 0.20 to 0.35 m below the surface. A number of studies have been conducted to determine the benefits of in-row subsoiling and results have been contradictory. The objective of this study was to evaluate the relationships between in-row subsoil and non-subsoil tillage treatments, soil water, and corn grain yields.
The study was conducted for two years on an Orangeburg sandy loam (Typic Paleudult). The study contained irrigated and non-irrigated treatments. The four tillage treatments used were (T1) in-row subsoiler followed by a double disk bedder, (T2) double disk bedder, (T3) fluted coulter followed by in-row subsoiler and slot filler tines, and (T4) fluted coulter. Tillage and planting were accomplished simultaneously. Each corn (Zea Mays L. ‘Dekalb XL72B’) crop was preceded by fall-planted wheat and the wheat (Triticum aestivium L. “Coker 747”) was killed with herbicides in the spring before corn planting. Wheat mulch was disked in prior to the bedding treatments and left undisturbed for the two fluted coulter treatments. Corn was planted 0.04 m deep with double disk openers. Soil water potential was maintained above 0.05 MPa in the irrigated corn plots. Forty kg/ha of N was applied at planting and followed 42 days later with eight weekly applications of 50 kg/ha N.
In-row subsoiling and irrigation treatments significantly increased grain yields. Irrigated corn grain yields were 12333 and 7872 kg/ha in 1978 and 1979, respectively. Non-irrigated corn yields were 7697 and 4892 kg/ha in 1978 and 1979, respectively. In-row subsoiled to a depth of 0.36 m and non-subsoiled grain yields were 8577 and 7820 kg/ha, respectively. There was no significant difference between bedding and fluted coulter treatments.
[1]
D. K. Cassel,et al.
Conservation tillage in the Southeast
,
1977
.
[2]
R. H. Shaw,et al.
The Effects of Soil Moisture Stress at Different Stages of Growth on the Development and Yield of Corn1
,
1960
.
[3]
N. A. Minton,et al.
Soybean Yields and Lance Nematode Populations as Affected by Subsoiling, Fertility, and Nematicide Treatments1
,
1975
.
[4]
H. M. Taylor,et al.
Effect of Soil Temperature, Strength, and pH on Cotton Seedling Root Elongation1
,
1970
.
[5]
C. R. Camp,et al.
Effect of Mechanical Impedance on Cotton Root Growth
,
1968
.
[6]
C. Phene,et al.
High-frequency Irrigation for Water Nutrient Management in Humid Regions1
,
1976
.
[7]
H. M. Taylor,et al.
Radicle Elongation of Pea Seedlings as Affected by Oxygen Concentration and Gradients between Shoot and Root 1
,
1971
.
[8]
Howard M. Taylor,et al.
PENETRATION OF COTTON SEEDLINGN TAPROOTS AS INFLUENCED BY BULK DENSITY, MOISTURE CONTENT, AND STRENGTH OF SOIL
,
1963
.
[9]
J. S. Robins,et al.
Some Effects of Severe Soil Moisture Deficits at Specific Growth Stages in Corn1
,
1953
.
[10]
W. G. Fleming,et al.
Nitrogen requirements associated with improved conservation tillage for corn production
,
1981
.
[11]
K. Barley,et al.
The influence of soil strength on the penetration of a loam by plant roots
,
1965
.