Crust-breaking device improves water infiltration into furrows
Shrini K. Upadhyaya, UC Davis
J. Jafari Far, UC Davis
Sayedahmad Shafii, UC Davis
H. Abdel Fattah, UC Davis
California Agriculture 51(5):21-22. DOI: 10.3733/ca.v051n05p21.
S.K. Upadhyaya is Professor, Department of Biological and Agricultural Engineering, UC Davis; J.J. Far is Visiting Researcher, Department of Biological and Agricultural Engineering, UC Davis; S. Shafii is Postgraduate Researcher, Department of Biological and Agricultural Engineering, UC Davis; H.A. Fattah is Graduate Assistant, Department of Biological and Agricultural Engineering, UC Davis;
Surface irrigation may lead to thick depositional crusts at the soil surface, which can reduce infiltration rate. To break the crust on the sides of the bed near the bottom of a furrow, we developed a torpedo-shaped, winged cultivator. Field experiments were conducted on a tomato crop at UC Davis on Yolo loam soil during the summer of 1992. Breaking the crust with the device increased cumulative infiltration significantly, by almost 30%.
A torpedo-shaped, winged crust-breaking device crushes through the crust on the soil surface in a tomato field. Inset, soil crusting impedes water penetration.
Electrical energy used in irrigating crops is 12% of the total energy required by California agriculture. Nearly 95% of the energy fueling irrigation pumps is supplied by electric motors, accounting for almost 68% of the direct electrical energy used by California agriculture — approximately 7 billion kWh. About 43% of this energy is used for pumping water out of the ground, and another 31 % is used for moving water from the supply source to the field. The remaining 26% is used to pressurize irrigation systems for applying water to the crop. Slow water penetration can lead to longer irrigation time to satisfy crop requirements, causing more evaporation and deep percolation while moving water from the source to the field. These losses reduce irrigation efficiency.
Soil crusting and compaction are the two major physical factors that impede water penetration into the soil. According to the 1984 Land Air and Water Resources Department report Water Penetration Problems in California Soils, slow water penetration is a major problem in the production of crops on over 2.5 million acres, or more than 20% of the irrigated land in California. Annual dollar losses are estimated to be from $20/acre in irrigated pasture to $500/acre in some orchards. Soils of all textures, from sandy loams to clays, have water-penetration problems. Slow water penetration into soils has the direct effect of reducing yields if plants become water stressed due to insufficient available water. Also, conveyance loss is increased while moving the water from the source to the field, thus increasing irrigation water requirements. The problem is particularly serious in light of the increasing urban demand for water, coupled with depletion of groundwater.
Infiltration can be substantially increased if the depositional crust at the bottom of the furrow is broken with a crust breaker. Enhanced infiltration rate reduces irrigation time, which in turn reduces conveyance losses when moving the water from source to the field, ultimately reducing pumping energy requirements. Moreover, additional savings in labor can be achieved.
The objectives of this study were (1) to develop a crust-breaking device to destroy the depositional crust near the bottom of the furrow in a furrow-irrigated field, and (2) to investigate the effect of destroying the depositional crust formed by furrow irrigation on infiltration characteristics of soil in a tomato field.
We designed a torpedo-shaped, winged device to break the depositional crust near the bottom of the furrow on both sides. Two of the crust-breaker units were fabricated and attached to a tool bar using cultivator shanks 2 inches wide by 1/2 inch thick (51 mm by 12 mm). Right-handed and left-handed beet hoes about 9 inches (225 mm) long were attached to a steel pipe about 6 inches (150 mm) in diameter and 1/4 inch (6 mm) thick. The front 7 1/2-inch (190 mm) length of the pipe was tapered to form a pointed cone. Total length of this unit was about 22 1/2 inches (572 mm).
TABLE 1. Experimental infiltration rate data obtained In a Yolo loam field planted to tomato crop during summer 1992
During operation, the hoes cut through the depositional crust near the bottom of the furrow on both sides. The total width of the crust breaker's cut was about 24 inches (610 mm). The shape of the crust breaker is such that it tends to firm the furrow bottom and reduce infiltration through it, an arrangement that may enhance the intake of water through the sides and into the bed.
On the UC Davis campus, we divided an area about 321 feet by 200 feet (98 m by 61 m) on a Yolo loam soil (Typic Xerorthents) into four blocks (main plots) of about 79 feet by 200 feet (24 m by 61 m) each. This was used for field tests during the 1991 and 1992 growing seasons. Each main plot was further divided into two subplots. The furrows in one of these subplots were assigned to the crust-breaking action of the torpedo-shaped winged cultivator (the cultivated subplot), while the furrows in the other subplot were left undisturbed (the uncultivated subplot).
Gated pipes were used to irrigate the field. Four subplots were fed by one valve and the other four subplots were fed by a second valve. A flow meter was used to measure the output of each valve. Each subplot had seven tomato beds and eight furrows. Three furrows in each subplot were randomly chosen for an inflow-outflow study. Four of the eight scheduled irrigations were selected for infiltration measurements. Before each of these four irrigations, the crust breaker was used to break the depositional crusts at the bottom of the furrows in cultivated subplots.
We used the results of the field tests conducted during the 1991 growing season to evaluate the design of the crust-breaker device and modify it as necessary. We found a significant increase in infiltration rate (18% to 59%) when the depositional crust was broken with a crust breaker. In our first design, cultivator tines attached in a V shape to the torpedo were located about 3 inches (75 mm) from the bottom of the torpedo. Our field tests indicated that this type of arrangement leads to a smooth channel at the bottom of the furrow, allowing the water to advance down the furrow quickly. This rapid advance reduces the advantage of breaking the depositional crust. In the second year of the study, the crust breaker was slightly modified so that the wing-shaped cultivator tines were at the same level as the bottom of the torpedo.
The lowest increase in mean infiltration rate (the ratio of cumulative infiltration to total irrigation time) resulting from cultivating with the crust breaker was 14.7% for the Aug. 14, 1992, irrigation, and the highest increase (43.4%) occurred for the June 16, 1992, irrigation (table 1). The overall mean increase was 29.6%. An analysis of variance of the infiltration data indicated that the time of irrigation and cultivation influenced infiltration data because of seasonal variability in infiltration and cultivation practice respectively.
The effect of cultivation on increasing infiltration was highly significant (P < 0.0006). Thus it is clear that cultivation with the crust breaker is helpful in enhancing infiltration if the waterpenetration problem is related to the depositional crust at the bottom of the furrow.
It should be noted that the crust-breaking operation requires an average of approximately 0.45 kWh/acre of energy, whereas the savings in irrigation energy requirements owing to reduced losses in transporting the water from the source to the field are approximately 3.4 kWh/acre for the tomato crop in the Central Valley. It is not practical to have a separate crust-breaking operation prior to each irrigation event. However, the crust-breaking operation can easily be combined with other operations, such as field cultivations (normally two to three), sidedressing and/or post-emergence herbicide application.
Tomato yield data obtained in each of the subplots were based on two measurements of yield on a bed about 10 feet (3 m) long. These yields are quite high, ranging from 33 tons/ acre to 41 tons/acre, with a mean of 37.5 tons/acre. We did not attempt to correlate the yield data with the crust-management technique (cultivated versus uncultivated), because we did not alter the irrigation practice to account for infiltration differences.
Based on the results of this study, we reached the following conclusions: