摘要
为研究地膜覆盖与灌水对棉田蒸散量及水热状况的影响,开展测坑和桶栽试验,设置三个灌水水平:3360(W1)、4200(W2)、5040 m^(3)·hm^(-2)(W3);两种地膜覆盖方式:覆膜(P1)和裸土(P2)。结果表明:(1)覆膜能有效降低棉花全生育期总蒸散量,W1、W2、W3灌溉水平下,覆膜处理棉花蒸散量分别降低25.31%、25.39%、25.75%。灌水量与蒸散量呈正相关关系,P1方式下,W3处理比W1、W2处理棉花蒸散量分别提高8.71%、7.50%;P2方式下,W3处理比W1、W2处理棉花蒸散量分别提高8.82%、8.02%。(2)覆膜能改变棉田土壤水热状况,可有效提高土壤温度和土壤含水率,覆膜对土壤水热状况的影响随土壤深度的增加而减弱;土壤温度与灌水量呈负相关关系,土壤含水率与灌水量呈正相关关系。(3)土壤含水率对裸土处理棉花蒸散量的相关系数影响最大,并随着土层深度的增加而降低;土壤温度对棉花蒸散量的相关系数随土层深度增加而升高,P1处理在20 cm土层相关系数最高,P2处理则在25 cm土层最高。探索覆膜滴灌对干旱区农田蒸散过程的影响对理解绿洲水文循环过程具有重要的理论意义,同时也可为干旱区有限水资源合理利用提供科学参考。
To examine the effects of plastic film coverage and irrigation on evapotranspiration as well as water and heat conditions in cotton fields,pit and barrel planting experiments were conducted.The experiments involved three irrigation levels:3360 m^(3)·hm^(-2)(W1),4200 m^(3)·hm^(-2)(W2),and 5040 m^(3)·hm^(-2)(W3),along with two plastic film covering methods:covered with film(P1)and bare soil(P2).The evapotranspiration pattern and soil water and heat status of drip irrigated cotton fields were analyzed.The results showed that:(1)Plastic film mulching effectively reduced the total evapotranspiration of cotton throughout the entire growth period.Under W1,W2,and W3 irrigation levels,the plastic film mulching treatment reduced cotton evapotranspiration by 25.31%,25.39%,and 25.75%,respectively.The irrigation amount was positively correlated with evapotranspiration.Under P1 mode,the cotton evapotranspiration of W3 treatment increased by 8.71%and 7.50%compared to W1 and W2 treatments,respectively.Under P2 mode,the cotton evapotranspiration of W3 treatment increased by 8.82%and 8.02%,respectively.(2)Film mulching had a considerable impact on the soil temperature and moisture content of the cotton fields,leading to an increase in soil temperature and moisture content.However,the impact of film mulching on soil water and thermal conditions diminished as soil depth increased.Additionally,there was a negative correlation between soil temperature and irrigation amount,and a positive correlation between soil moisture content and irrigation amount.(3)Soil moisture content was found to have the greatest influence on the correlation coefficient of cotton evapotranspiration in the bare soil treatment,and it decreased with increasing soil depth.On the other hand,the correlation coefficient of soil temperature on cotton evapotranspiration increased with soil depth.It is worth noting that the P1 treatment had the highest correlation coefficient in the 20 cm soil layer,while the P2 treatment had the highest correlation coefficient in the 25 cm soil layer.Exploring the impact of film mulching and drip irrigation on the evapotranspiration process of farmland under water-saving conditions in arid regions is of great theoretical significance.This research helps in understanding the hydrological cycle and stability mechanisms of oases.Additionally,it provides valuable scientific insights for optimizing and utilizing limited water resources in arid areas.
作者
刘承岳
杨广
郭明华
贾伟康
孔春贤
王春霞
何新林
张硕
赵丽
李鹏飞
蒲胜海
LIU Chengyue;YANG Guang;GUO Minghua;JIA Weikang;KONG Chunxian;WANG Chunxia;HE Xinlin;ZHANG Shuo;ZHAO Li;LI Pengfei;PU Shenghai(College of Water Conservancy&Architectural Engineering,Shihezi University,Shihezi,Xinjiang 832003,China;Key Laboratory of Cold and Arid Regions Eco-Hydraulic Engineering of Xinjiang Production&Construction Corps,Shihezi,Xinjiang 832003,China;Water Conservancy Project Management and Service Center of Shihezi,Shihezi,Xinjiang 832000,China;Research Institute of Soil,Fertilizer and Agricultural Water Conversation,Xinjiang Academy of Agricultural Sciences/Key Laboratory of Agro-Environment in Northwest Oasis,Ministry of Agriculture and Rural Affairs,Urumqi,Xinjiang 830091,China)
出处
《干旱地区农业研究》
CSCD
北大核心
2024年第6期172-180,215,共10页
Agricultural Research in the Arid Areas
基金
国家自然科学基金项目(52269006)
新疆生产建设兵团科技项目(2022BC001,2022DB023,2023AB059)
石河子市科技计划项目(2023NY01)
第三次新疆综合科学考察项目(2021xjkk0804)
农业科技创新稳定支持项目(xjnkywdzc-2023005-6)
国家重点研发计划项目(2021YFD1900803)。
关键词
棉花
滴灌
覆膜
蒸散发
土壤含水率
土壤温度
cotton
drip irrigation
mulching
evapotranspiration
soil moisture
soil temperature