首页> 外文期刊>Agricultural Water Management >Drying/rewetting cycles of the soil under alternate partial root-zone drying irrigation reduce carbon and nitrogen retention in the soil-plant systems of potato.
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Drying/rewetting cycles of the soil under alternate partial root-zone drying irrigation reduce carbon and nitrogen retention in the soil-plant systems of potato.

机译:在交替的部分根区干燥灌溉下,土壤的干燥/再湿循环减少了马铃薯在土壤-植物系统中的碳和氮保留。

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Dry/wet cycles of soil may stimulate mineralization of soil organic carbon (C) and nitrogen (N) leading to increased N bioavailability to plants but potentially also increased C and N losses. We investigated the effects of partial root-zone drying (PRD) and deficit irrigation (DI) on C and N retention in the soil-plant systems of potato. Potato plants were grown in 20 L split-root pots with three N-fertilization rates, viz., 1.4 (N1), 2.5 (N2), and 4 (N3) g N pot-1 soil, respectively. At tuber initiation and earlier tuber bulking stages, the plants were subjected to PRD and DI treatment for five weeks. For each N rate, the PRD and DI plants received a same amount of water, which allowed re-filling one half of the PRD pots close to full water holding capacity. The results showed that plant dry biomass, plant water use, and water use efficiency were increased with increasing N-fertilization rate but were unaffected by the irrigation treatment. As compared with DI, PRD significantly decreased soil C and N contents, which could have been due to an enhanced soil organic C and N mineralization. PRD did not influence plant C content but significantly increased plant N content in relation to DI. However, owing to substantial decreases of C and N contents in the soil, the amounts of C and N retained in the soil-plant systems were lower in PRD than in DI. Although the C gain in the soil-plant systems of potato was positive due to production of plant biomass, the dry/wet cycles of the soil under the PRD treatment stimulated the mineralization of soil organic C and N leading to greater C and N losses; thus PRD might not be a sustainable irrigation practice in terms of C and N sequestration in the soil-plant systems.
机译:土壤的干/湿循环可能会刺激土壤中有机碳(C)和氮(N)的矿化,从而增加植物对氮的生物利用度,但也可能增加碳和氮的损失。我们调查了部分根区干燥(PRD)和亏缺灌溉(DI)对马铃薯土壤-植物系统中碳和氮保留的影响。马铃薯植物种植在20升分叉盆中,氮肥施用量为3种,分别为1.4(N1),2.5(N2)和4(N3)g N pot -1 土壤,分别。在块茎萌发和早期块茎膨大阶段,对植物进行PRD和DI处理5周。对于每一个N比率,珠三角和DI厂都接受相同量的水,从而可以将一半的珠三角盆重新注水至接近满水容量。结果表明,随着氮肥用量的增加,植物干生物量,植物水分利用和水分利用效率均得到提高,但不受灌溉处理的影响。与DI相比,PRD显着降低了土壤中的C和N含量,这可能是由于土壤有机C和N矿化作用增强所致。珠三角不影响植物C含量,但相对于DI而言,植物N含量显着增加。但是,由于土壤中碳和氮含量的显着降低,珠三角地区土壤-植物系统中保留的碳和氮含量低于去离子土壤。尽管由于植物生物量的产生,马铃薯在土壤-植物系统中的碳增加为正,但在珠三角处理下土壤的干/湿循环刺激了土壤有机碳和氮的矿化,导致更大的碳和氮损失。因此,就土壤-植物系统中的碳和氮固存而言,珠三角可能不是可持续的灌溉方式。

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