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Stable isotope analysis of water extraction from subsoil in upland rice (Oryza sativa L.) as affected by drought and soil compaction

机译:受干旱和土壤压实影响的旱稻(Oryza sativa L.)底土中水提取的稳定同位素分析

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Water extraction from subsoil in upland rice (Oryza sativa L.) was examined as related to topsoil desiccation and subsoil compaction. The water extraction was observed by measurements of heavy water concentrations in transpiring plants. The plants were grown in pots that were filled with sandy soil and vertically compartmented into two columns. Heavy water was applied to the subsoil. Plants exposed to mild topsoil desiccation (−120 kPa in water potential) eventually increased water extraction from the subsoil and maintained photosynthetic rate and stomatal conductance at the wet condition level. The rates of the plants subjected to severely droughted topsoil (−190 kPa) were significantly lowered due to less water uptake from the subsoil. Subsoil compaction at bulk densities of 1.45 and 1.50 Mg m−3 inhibited increase of root length densities. Limited water extraction from the subsoil was insufficient to maintain plant productivity under drought conditions. Daily water uptake per unit of root length in the lower tube did not apparently increase even if water demand on the unit root length increased. When water to topsoil was completely withheld, water extraction from the subsoil gradually increased as the topsoil dried out. Plants that were watered and rewatered took up very little water from the subsoil. The extraction from the subsoil occurred only when water potential of the topsoil was below about −190 kPa.
机译:研究了从旱稻(Oryza sativa L.)的地下土壤中提取水分与表层土壤干燥和地下土壤压实有关。通过测量蒸腾植物中的重水浓度来观察水的提取。将植物种植在装满沙土的花盆中,并垂直分隔成两列。将重水施加到下层土壤上。暴露于轻度表土干燥(水势为-120 kPa)的植物最终增加了从下层土壤的水分提取,并在潮湿条件下保持了光合速率和气孔导度。由于底土的吸水量减少,遭受严重干旱的表土(-190 kPa)的植物的比率显着降低。在1.45 Mg m-3和1.50 Mg m-3 的堆积密度下进行的次土压实抑制了根长密度的增加。从地下土壤中提取有限的水分不足以在干旱条件下维持植物的生产力。即使对单位根长的需水量增加,下管中每单位根长的每日吸水量也没有明显增加。当完全阻止表层土壤中的水时,随着表层土壤干out,从地下土壤中提取的水逐渐增加。经过浇水和再浇水的植物从土壤中吸收的水分很少。仅当表层土壤的水势低于约-190 kPa时才从地下土壤中提取。

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