Wheat root growth responses to horizontal stratification of fertiliser in a water-limited environment
Wheat root growth responses to horizontal stratification of fertiliser in a water-limited environment
复制标题
限水环境下小麦根系生长对肥料水平分层的响应
DOI:
10.1007/s11104-014-2249-8
复制
发表时间:
2015-01-01
期刊:
影响因子:
4.9
通讯作者:
Whalley, William R.
中科院分区:
文献类型:
--
作者:
Jin, Kemo;Shen, Jianbo;Whalley, William R.
Background and aimsWe were interested to determine the effects of horizontal stratification of nutrient-rich zones within different layers of the soil profile in water-limited environments on root growth and crop yield. This is practically relevant to large areas of China, many of which have been over-fertilized.MethodsWe used soil-filled rhizotrons 1.4 m deep to grow wheat. Three different nutrient-rich horizontal stratifications were used at depths of 0–40, 60–100 and 0–140 cm. The soil was packed to a density of 1.5 g cm−3, at a matric potential of −10 kPa. The wheat was grown until it was at terminal drought. Low soil hydraulic conductance preserved the horizontal nutrient stratification.ResultsPlants grown in rhizotrons with a surface layer (0–40 cm) of nutrients had the greatest root growth, water uptake and yield. When nutrients were uniformly distributed throughout the rhizotron (0–140 cm), root growth was restricted to the surface layer. Measurements of soil moisture indicate this was because the roots became impeded.ConclusionsNutrient enrichment of the surface layer was the most effective at promoting deep roots, higher water uptake and yield under water-limited conditions. Heterogeneous nutrient distribution can modify root growth and water uptake.