首页|期刊导航|水土保持研究|咸淡水组合灌溉下鲁北盐碱土壤水盐分布及脱盐特征

咸淡水组合灌溉下鲁北盐碱土壤水盐分布及脱盐特征OA

Water-salt distribution and desalination characteristics of saline-alkali soils under combined irrigation of brackish-fresh water in Northern Shandong

中文摘要英文摘要

[目的]揭示微咸水淡化灌溉对盐碱土壤水盐的调控效果,为鲁北地区破解农业淡水资源短缺与土壤盐碱化问题提供安全的微咸水灌溉方案.[方法]以取自垦利区的重度盐碱化土壤为对象,借助室内土柱模拟试验与一维代数模型,探究不同咸淡水组合比例(全部淡水和微咸水灌溉以及咸∶淡=1∶2,1∶1,2∶1)和次序(先咸后淡和先淡后咸)下土壤水盐分布及脱盐特征.[结果]随着咸淡水组合比例的提高,同一土层的土壤含水率先升高后降低,其中在5-15 cm土层,咸∶淡=1∶2的土壤含水率最高,在15-55 cm土层,咸∶淡=2∶1的土壤含水率最高.相较于先淡后咸,先咸后淡提高了土壤含水率.对于土壤水分垂直分布,一维代数模型模拟效果"极好",标准化均方根误差小于10%,一致性指数大于0.9.在5-35 cm,5-25 cm和5-15 cm土层,咸∶淡=1∶2,1∶1,2∶1的土壤含盐量分别小于全部微咸水灌溉,与全部淡水灌溉一致.所以在一定土层内,咸淡水组合灌溉产生了与全部淡水灌溉相同的脱盐作用,尤其当咸∶淡=1∶2时,达标土壤脱盐深度与全部淡水灌溉下的情况差异不显著.先咸后淡对浅层(5-10 cm)的脱盐效果更明显,而先淡后咸对深层(40-45 cm)的脱盐效果更明显.[结论]综合考虑不同咸淡水组合比例和次序的影响,建议选择1∶2的咸淡水组合比例和先咸后淡的咸淡水组合次序.

[Objective]This study aims to reveal the regulatory effects of diluted brackish water irrigation on water and salt dynamics in saline-alkali soil in Northern Shandong and to provide a safe irrigation scheme to alleviate agricultural freshwater shortage and soil salinization-alkalization.[Methods]Severely saline-alkali soils collected from the Kenli District were used in this study.Laboratory-based soil column simulation experiments and a one-dimensional algebraic model were used to investigate soil water-salt distribution and desalination characteristics under different combination ratios and irrigation sequences of brackish and fresh water.The five combination ratios were:all fresh water,all brackish water,and brackish-to-fresh water ratios of 1∶2,1∶1,and 2∶1.Two sequences were:brackish water irrigated before fresh water and fresh water irrigated before brackish water.[Results]As the combination ratio of brackish-to-fresh water increased,the soil water content in the same soil layer initially increased and then decreased.The highest soil water content was observed in the 5-15 cm layers under the brackish-to-fresh water ratio of 1∶2 and 15-55 cm layers under the ratio of 2∶1.Compared with the fresh water-first sequence,applying brackish water before fresh water resulted in higher soil water content.The one-dimensional algebraic model performed excellently in simulating vertical soil water distribution,with a normalized root mean square error<10%and an index of agreement>0.9.Soil salt content under the 1∶2,1∶1,and 2∶1 brackish-to-fresh water ratios,was lower than that under brackish water irrigation alone,and was consistent with that under fresh water irrigation alone in soil layers of 5-35 cm,5-25 cm,and 5-15 cm,respectively.Therefore,combined irrigation of brackish and fresh water produced the same desalination effect as using only fresh water in certain soil layers,especially under the 1∶2 brackish-to-fresh water ratio,where the effective desalination depth showed no significant difference from that produced by fresh water irrigation alone.Applying brackish water before fresh water was more effective for soil desalination in shallow soil layers(5-10 cm),whereas the fresh water-first sequence was more effective in deep soil layers(40-45 cm).[Conclusion]Considering both combination ratios and irrigation sequences,a brackish-to-fresh water ratio of 1∶2 combined with the irrigation sequence of brackish water first and then fresh water is recommended.

王乃江;李嘉怡;武华宝;王伟臣;高佩玲;刘璐

山东农业工程学院 国土资源与测绘工程学院,济南 250100潍坊学院 现代农学院,山东 潍坊 261061山东农业工程学院 国土资源与测绘工程学院,济南 250100山东农业工程学院 国土资源与测绘工程学院,济南 250100山东理工大学 资源与环境工程学院,山东 淄博 255000山东农业工程学院 国土资源与测绘工程学院,济南 250100

农业科技

盐碱土壤咸淡水组合灌溉模拟试验土壤水盐分布土壤脱盐

saline-alkali soilcombined irrigation of brackish and fresh watersimulation experimentsoil water-salt distributionsoil desalination

《水土保持研究》 2026 (3)

257-265,9

山东省自然科学基金资助项目(ZR2025QC543)山东农业工程学院高层次人才科研启动经费资助项目(2024GCCZR-09)山东省大学生创新创业训练计划项目(S202411067040)

10.13869/j.cnki.rswc.2026.03.004

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