Paudel Indira, Cohen Shabtai, Shaviv Avi, Bar-Tal Asher, Bernstein Nirit, Heuer Bruria, Ephrath Jhonathan
Institute of Soil, Water and Environmental Sciences, ARO Volcani Center, Bet Dagan 50250, Israel The Robert H. Smith Faculty of Food Agriculture and Environment, The Hebrew University of Jerusalem, Rehovot 76100, Israel.
Institute of Soil, Water and Environmental Sciences, ARO Volcani Center, Bet Dagan 50250, Israel
Tree Physiol. 2016 Jun;36(6):770-85. doi: 10.1093/treephys/tpw013. Epub 2016 Mar 28.
Roots interact with soil properties and irrigation water quality leading to changes in root growth, structure and function. We studied these interactions in an orchard and in lysimeters with clay and sandy loam soils. Minirhizotron imaging and manual sampling showed that root growth was three times lower in the clay relative to sandy loam soil. Treated wastewater (TWW) led to a large reduction in root growth with clay (45-55%) but not with sandy loam soil (<20%). Treated wastewater increased salt uptake, membrane leakage and proline content, and decreased root viability, carbohydrate content and osmotic potentials in the fine roots, especially in clay. These results provide evidence that TWW challenges and damages the root system. The phenology and physiology of root orders were studied in lysimeters. Soil type influenced diameter, specific root area, tissue density and cortex area similarly in all root orders, while TWW influenced these only in clay soil. Respiration rates were similar in both soils, and root hydraulic conductivity was severely reduced in clay soil. Treated wastewater increased respiration rate and reduced hydraulic conductivity of all root orders in clay but only of the lower root orders in sandy loam soil. Loss of hydraulic conductivity increased with root order in clay and clay irrigated with TWW. Respiration and hydraulic properties of all root orders were significantly affected by sodium-amended TWW in sandy loam soil. These changes in root order morphology, anatomy, physiology and hydraulic properties indicate rapid and major modifications of root systems in response to differences in soil type and water quality.
根系与土壤性质和灌溉水质相互作用,导致根系生长、结构和功能发生变化。我们在果园以及装有黏土和砂壤土的蒸渗仪中研究了这些相互作用。微根窗成像和人工采样表明,相对于砂壤土,黏土中的根系生长速度低三倍。经处理的废水(TWW)使黏土中的根系生长大幅减少(45 - 55%),但砂壤土中未出现这种情况(<20%)。经处理的废水增加了盐分吸收、膜渗漏和脯氨酸含量,并降低了细根中的根系活力、碳水化合物含量和渗透势,尤其是在黏土中。这些结果证明经处理的废水对根系系统构成挑战并造成损害。在蒸渗仪中研究了不同根序的物候和生理特征。土壤类型对所有根序的直径、比根面积、组织密度和皮层面积影响相似,而经处理的废水仅对黏土中的这些指标有影响。两种土壤中的呼吸速率相似,黏土中的根系水力传导率严重降低。经处理的废水增加了黏土中所有根序的呼吸速率并降低了其水力传导率,但仅降低了砂壤土中较低根序的水力传导率。在黏土以及用经处理的废水灌溉的黏土中,水力传导率的损失随根序增加。在砂壤土中,经钠改良的经处理的废水显著影响了所有根序的呼吸和水力特性。根序形态、解剖结构、生理特征和水力特性的这些变化表明,根系系统会因土壤类型和水质的差异而迅速发生重大改变。