Influence of soil strength on wheat (Triticum aestivum) growth under prolonged tillage

K. Priya, I. Mani, R. A. Parray, P. Sahoo, D. K. Singh, K. Bandyopadhyaya, S. Sarkar
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Abstract

Tillage enhances soil physical condition which favors root growth and crop productivity. Though, continuous rotary tillage at same depth leads to the formation of plough pan which slowdown crop productivity. Some serious speculations have been made about rotary tillage that in long run it induces subsoil compaction. This study was conducted at farmers’ field in Malhendi , Shamli (UP) to investigate the effect of prolonged use of rototilling with special attention to subsoil compaction. The experimental sites were under rotary tillage (RT) under wheat for last 15 years under rice-wheat cropping system which compared with conventional tillage (CT-cultivator harrow). The crop growth and yield was reduced under RT due high mechanical impedance and BD in deeper layer as compared to CT. In upper soil strata (5-15 cm) the cone index of RT (505kPa-2057kPa) soils are lesser than that of CT (625-2257kPa) while in subsoil layer (45cm) it becomes severe under RT(4578 kPa) compared to CT (2468 kPa). Similar trend found in bulk density under both tillage treatments. The bulk densities observed before tillage at 0-15cm, 15-30 and 30-45cm depth were 1.50 Mg/m3 and 1.56 Mg/m3,1.37 Mg/m3 for CT 1.42 Mg/m3 1.67 Mg/m3 and 1.81 Mg/m3 for RT respectively. The grain yields were (5909 kg/ha) and (4594 kg/ha) under CT and RT tillage system respectively. The CT system well performed in plant height, no of tillers and root growth characteristics, viz. root length density, root volume than that of RT. Performing studies shows that long-term RT induced subsoil compaction which needs some amelioration tillage management.
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长期耕作条件下土壤强度对小麦生长的影响
耕作改善了土壤的物理条件,有利于根系生长和作物生产力。然而,在同一深度连续轮作会导致犁盘的形成,从而降低作物产量。有人严肃地猜测,从长远来看,旋耕法会导致底土压实。本研究在沙姆利(UP) Malhendi的农民田间进行,以调查长期使用旋耕法并特别注意底土压实的效果。试验场地连续15年采用小麦轮作(RT),与常规耕作方式(ct -耕耘机耙)进行比较。与连续耕相比,由于机械阻抗高,且耕层较深,导致作物生长和产量下降。在表层(5 ~ 15 cm), RT(505kpa ~ 2057kpa)土壤的锥指数小于CT (625 ~ 2257kpa),而在底层(45cm), RT(4578 kPa)下锥指数大于CT (2468 kPa)。两种耕作方式的容重变化趋势相似。耕前0 ~ 15cm、15 ~ 30、30 ~ 45cm深度容重分别为1.50 Mg/m3、1.56 Mg/m3、1.37 Mg/m3、1.42 Mg/m3、1.67 Mg/m3、1.81 Mg/m3。轮作和轮作的产量分别为5909 kg/ha和4594 kg/ha。连续耕制在株高、分蘖数和根系生长特征(根长密度、根体积)方面均优于对照耕制。研究表明,长期连续耕制会导致土壤压实,需要对耕作管理进行一定的改进。
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