内蒙古农业大学水利与土木建筑工程学院,呼和浩特,010018
[ "李俊杰(1997—),男,硕士研究生,主要从事盐碱地改良与水资源高效利用研究。E-mail:762636913@qq.com" ]
纸质出版:2023
移动端阅览
李俊杰, 屈忠义, 杨威, 等. 咸水结冰灌溉下盐碱地土壤水热盐动态迁移特征分析[J]. 水土保持学报, 2023,37(2):377-384.
LI Junjie, QU Zhongyi, YANG Wei, et al. Analysis of Dynamic Migration Characteristics of Soil Water, Heat, and Salt in Saline-alkali Soils Under Saline Water Freezing Irrigation[J]. 2023, 37(2): 377-384.
李俊杰, 屈忠义, 杨威, 等. 咸水结冰灌溉下盐碱地土壤水热盐动态迁移特征分析[J]. 水土保持学报, 2023,37(2):377-384. DOI: 10.13870/j.cnki.stbcxb.2023.02.044.
LI Junjie, QU Zhongyi, YANG Wei, et al. Analysis of Dynamic Migration Characteristics of Soil Water, Heat, and Salt in Saline-alkali Soils Under Saline Water Freezing Irrigation[J]. 2023, 37(2): 377-384. DOI: 10.13870/j.cnki.stbcxb.2023.02.044.
为探究合理的咸水结冰灌溉水量及咸水结冰灌溉下冻融期土壤水热盐动态迁移规律
以重度盐碱地为研究对象
在内蒙古达拉特旗开展连续2年田间小区原位冻融试验
设置4组灌水梯度
灌水量分别为140 mm (S1)
180 mm (S2)
220 mm (S3)以及不进行灌溉对照(CK)
灌溉水矿化度为8~10 g/L。通过测定试验期内土壤含水率、土壤温度以及盐分分布
分析咸水结冰灌溉下盐碱地土壤水热盐动态迁移特征。结果表明:咸水结冰灌溉可显著提高春季消融后土壤含水率
减缓冻融期深层土壤温度变异程度
降低因土壤温度变化引起的返盐现象
灌溉水量越大
土壤含水率提升幅度越大、保温效果越显著。经过反复冻融循环
适宜的咸水结冰灌溉处理下土壤盐分降低
当灌溉水量<180 mm时脱盐率与灌水量呈正相关
当灌水量>180 mm时春季消融后土壤含盐量增加。2年试验期内相较于未进行灌溉的对照处理
咸水结冰灌溉处理下土壤含水率提高82%~93%;土壤消融指数提高28%~65%;土壤冻结指数降低24%~25%;灌水量<180 mm时0—40 cm土层脱盐率最高可达59%。综合考虑
在不造成土壤积盐导致次生盐渍化的前提下
灌溉水量180 mm下土壤保温、保墒、脱盐效果最好
可为来年作物生长提供适宜的土壤环境。
In order to explore the reasonable amount of brackish water icing irrigation water and the dynamic migration of soil hydrothermal salt during freezing-thawing period under saline freezing irrigation
taking the severe saline and alkali land as the research object
an in-situ freezing-thawing experiment was carried out in Dalat Banner
Inner Mongolia for two consecutive years
and four irrigation gradients was set
with irrigation amount of 140 mm (S1)
180 mm (S2)
220 mm (S3) and the control (CK) without irrigation
respectively
the salinity of irrigation water was 8~10 g/L.By measuring soil moisture content
soil temperature and salinity distribution during the experimental period
the dynamic migration characteristics of soil hydrothermal salt in saline and alkaline land under saline ice irrigation were analyzed.The results showed that brackish water icing irrigation could significantly increase the soil moisture content after spring ablation
slow down the deep soil temperature variation degree during the freeze-thaw period
reduced the salinity phenomenon caused by soil temperature change
and the larger the irrigation water volume
the greater the increase of soil moisture content and the more significant the thermal insulation effect.After repeated freeze-thaw cycles
soil salinity was reduced under suitable brackish water icing irrigation treatment
and the desalination rate was positively correlated with the irrigation amount when the irrigation water amount was less than 180 mm
and the soil salinity content increased after spring ablation when the irrigation amount was more than 180 mm.During the 2-year experimental period
compared with the control treatment without irrigation
the soil moisture content under the brackish water icing irrigation treatment was increased by 82%~93%;the soil ablation index was increased by 28%~65%;the soil freezing index was reduced by 24%~25%;the desalination rate of 0—40 cm soil layer when the irrigation amount was less than 180 mm could reach up to 59%.Considering the comprehensive consideration
under the premise of not causing soil salt accumulation leading to secondary salinization
soil insulation
moisture preservation and desalination effect under irrigation water of 180 mm is the best
which can provide a suitable soil environment for crop growth in the coming year.
黄晶,孔亚丽,徐青山,等.盐渍土壤特征及改良措施研究进展[J].土壤,2022,54(1):18-23.
景宇鹏,连海飞,李跃进,等.河套盐碱地不同利用方式土壤盐碱化特征差异分析[J].水土保持学报,2020,34(4):354-363.
胡敏,屈忠义,王丽萍,等.不同改良剂对河套灌区盐渍化土壤性状和葵花生长特性的影响[J].水土保持学报,2019,33(5):316-322.
杨真,王宝山.中国盐碱地改良利用技术研究进展及未来趋势[J].水土保持,2014,2(1):1-11.
史海滨,杨树青,李瑞平,等.内蒙古河套灌区水盐运动与盐渍化防治研究展望[J].灌溉排水学报,2020,39(8):1-17.
王胡军,李纯,钟香梅,等.盐碱地改良技术研究进展[J].农业工程,2014,4(增刊1):44-47.
陈文,郑自宽,谢军健,等.我国非常规水源苦咸水资源及其分布特征研究[J].水文,2021,41(5):1-6.
郭凯,巨兆强,封晓辉,等.咸水结冰灌溉改良盐碱地的研究进展及展望[J].中国生态农业学报,2016,24(8):1016-1024.
隆小华,倪妮,金善钊,等.北方滨海盐碱地冬季咸水结冰灌溉对菊芋生长及离子分布的影响[J].农业环境科学学报,2012,31(1):161-165.
李宪,李亚光.不同矿化度咸水冬季结冰灌溉对滨海盐碱土的改良效果[J].中国水土保持科学,2015,13(3):64-68.
潘洁,肖辉,王立艳,等.咸水冰融化与土壤入渗过程不同盐分离子迁移规律研究[J].华北农学报,2012,27(1):210-214.
张秀梅,郭凯,谢志霞,等.冬季咸水结冰灌溉下滨海重盐碱地土壤水盐动态及对棉花出苗和产量的影响[J].中国生态农业学报,2012,20(10):1310-1314.
李志刚,刘小京,张秀梅,等.冬季咸水结冰灌溉后土壤水盐运移规律的初步研究[J].华北农学报,2008,23(增刊1):187-192.
张如鑫,屈忠义,王丽萍,等.生物炭对冻融期盐渍化土壤水热肥效应的影响[J].水土保持学报,2022,36(5):296-303.
李争争,屈忠义,杨威,等.不同矿化度咸水结冰灌溉对重度盐碱地土壤水分入渗和盐分运移的影响[J].水土保持学报,2021,35(3):304-311.
王全九.土壤物理与作物生长模型[M].北京:中国水利水电出版社,2016.
张美桃,杨培岭,任树梅,等.灌溉水盐分及灌水量对土壤水盐分布与春玉米生长的影响[J].水土保持学报,2022,36(4):290-298.
张越,杨劲松,姚荣江.咸水冻融灌溉对重度盐渍土壤水盐分布的影响[J].土壤学报,2016,53(2):388-400.
付强,侯仁杰,李天霄,等.冻融土壤水热迁移与作用机理研究[J].农业机械学报,2016,47(12):99-110.
潘大全,陈军锋,薛静,等.冻融期不同时间灌水对土壤水热影响的试验研究[J].节水灌溉,2022(1):1-6.
Kurz D, Alfaro M, Graham J. Thermal conductivities of frozen and unfrozen soils at three project sites in northern Manitoba[J].Cold Regions Science and Technology,2017,140(8):30-38.
付强,颜培儒,李天霄,等.冻融期不同覆盖和气象因子对土壤导热率和热通量的影响[J].农业工程学报,2017,33(20):98-105.
Zhang W, Yi Y, Jafarov E E, et al. Simulation of permafrost and seasonally frozen ground conditions and their response to recent climate warming in the Tibetan Plateau// Wen J Z. AGU Fall Meeting Abstracts. American,2015:14-18.
唐文政,王春霞,范文波,等.积雪与地表联合覆盖条件下冻融土壤水盐运移规律[J].水土保持学报,2017,31(3):337-343.
张殿发,郑琦宏,董志颖.冻融条件下土壤中水盐运移机理探讨[J].水土保持通报,2005,25(6):14-18.
Bing H, He P, Zhang Y. Cyclic freeze-thaw as a mechanism for water and salt migration in soil[J].Environmental Earth Sciences,2015,74(1):675-681.
Beier N, Sego D, Donahue R, et al. Laboratory investigation on freeze separation of saline mine waste water[J].Cold Regions Science and Technology,2007,48(3):239-247.
张璐,杨帆,王志春.咸水结冰灌溉融水淋盐改良盐渍土研究进展[J].土壤与作物,2021,10(2):202-212.
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