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Nutrient uptake by rice and soil solution composition under atmospheric CO2 enrichment

机译:大气CO2浓度升高下水稻和土壤溶液养分的吸收。

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Using free-air CO2 enrichment (FACE) we grew rice crops at ambient or elevated (ca. 250 mumol mol(-1) above ambient) and evaluated soil nutrition status by determining the elemental composition of soil solution. The dry matter of rice was increased by elevated CO2. Although the increase in dry matter after panicle initiation was greater in rice grown with FACE than in rice grown in ambient CO2, the increase rate was lower after panicle initiation. The nitrogen (N), phosphorus (P), potassium (K), and magnesium (Mg) concentrations of rice were significantly 21, 6, 14, and 9% lower, respectively, in rice grown with FACE than the concentrations in ambient grown rice at panicle initiation, and the N and K concentrations were significantly lower with FACE at harvest. Although the N and K uptakes of rice were higher with FACE than in ambient grown rice at panicle initiation, the differences were small after panicle initiation. The ammonium, phosphate, K, and silicate concentrations in soil solution gradually decreased before panicle initiation. The relation between the N and K uptake of rice and the concentrations in soil solution indicated the N and K supply from soil regulated the uptake after the concentrations were decreased in soil solution. The N uptake of rice appeared to be determined by the soil N availability, not by nutrition demand and uptake ability of rice after panicle initiation, and the amount of N uptake seemed to limit rice growth.
机译:使用自由空气CO2富集(FACE),我们在环境温度或升高温度(高于环境温度约250μmolmol(-1))下种植水稻作物,并通过确定土壤溶液的元素组成来评估土壤营养状况。二氧化碳的升高使稻米的干物质增加。尽管用FACE种植的水稻在穗开始后的干物质增加比在环境CO2中生长的水稻要大,但在穗开始后的增加率却较低。用FACE种植的水稻的氮(N),磷(P),钾(K)和镁(Mg)的浓度分别比环境生长的水稻低21、6、14和9%穗开始时,水稻的氮和钾浓度显着降低。虽然在穗开始时,用FACE处理的水稻对氮和钾的吸收高于在环境中种植的水稻,但穗开始后的差异很小。在穗开始之前,土壤溶液中的铵,磷酸盐,钾和硅酸盐浓度逐渐降低。水稻对氮,钾的吸收与土壤溶液浓度的关系表明,土壤溶液中氮,钾的供应量随土壤溶液浓度的降低而调节。水稻对氮的吸收似乎是由土壤氮的有效利用决定的,而不是由穗开始后的营养需求和水稻的吸收能力决定的,氮的吸收量似乎限制了水稻的生长。

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