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1)  Slight saline water irrigation mode
微咸水灌溉模式
2)  brackish water irrigation
微咸水灌溉
1.
Study on effect of brackish water irrigation on groundwater environment in arid area;
干旱区微咸水灌溉对地下水环境影响的研究
2.
Prediction of water-soil environment effect under brackish water irrigation in arid area;
干旱区微咸水灌溉的水-土环境效应预测研究
3)  light saline water irrigation
微咸水灌溉
1.
the filed experiment of slight saline water irrigation was carried out, and the influence of slight saline water concentration and rotation irrigation of fresh water and slight saline water on the crop growth and yield was analyzed based on the review of research results of slight saline water irrigation.
在结合国内外微咸水灌溉试验成果的基础之上,利用大田微咸水灌溉试验,分析了微咸水矿化度和咸淡轮灌次序对作物生长和产量的影响,研究结果表明小麦的产量随灌水矿化度的增加而减少,不同轮灌次序的咸淡轮灌试验结果表明,采用咸淡轮灌产量的大小次序为淡淡咸>咸淡咸>淡咸咸。
2.
But the soil still was belongs to the light salinity, and the light saline water irrigation couldn′t affect the soil water environment significantly.
利用识别后的SWAP模型,探讨了微咸水灌溉条件下土壤水盐及其均衡要素的转化关系和土壤的积盐趋势预测。
4)  saline water irrigation
微咸水灌溉
1.
Slight saline water irrigation systems for winter wheat;
冬小麦微咸水灌溉制度的研究
2.
The SWAP model was calibrated and validated with the collected experimental data,and the model was applied to evaluate the saline water irrigation scheduling for the experimental year and different hydrological years.
根据宁夏引黄灌区春玉米微咸水灌溉试验的数据结果,应用SWAP模型在田间尺度上对微咸水灌溉条件下春玉米田间土壤水盐运移规律和灌溉制度进行模拟,对拟定的各种灌溉方案进行评价。
5)  saline water irrigation
咸水灌溉
1.
On the basis of crop-water-salt production function and water-salt transport model,the maximum yield per unite area is taken as the target function to establish the model for saline water irrigation scheduling.
本文在作物水盐生产函数和农田水盐动态模型基础上,以单位面积纯收益最大为目标函数提出了制定咸水灌溉制度的模型。
2.
0 model was introduced systematically, and dynamic variation of environmental factors, crop growth and yield with light saline water irrigation were predicted.
0模型 ,预测了微咸水灌溉对土壤水盐动态、作物生长及产量等环境因子的动态变化 ,试验地点为内蒙古河套灌区红卫田间试验区 ,引用黄河水和高矿化度地下水混合进行灌溉。
3.
Based on field experiments of the saline water irrigation which have been conducted in the Hongwei Water Saving Demonstration Plot in Inner Mongolia Autonomous Region, SWAP(Soil-Water-Atmosphere-Plant) model developed by Wageningen Agricultural College was used as an analyzing tool.
以内蒙古河套灌区红卫节水示范园的咸水灌溉试验为基础,以荷兰Wageningen农业大学等单位开发的土壤—水分—大气—作物系统模拟软件SWAP为工具,应用示范园的土壤、水、盐分试验资料对模型的参数进行了率定和验证。
6)  Irrigation with saline water
咸水灌溉
1.
Effects of irrigation with saline water on soil salinity and crop yield;
微咸水灌溉对土壤盐分和作物产量影响研究
补充资料:咸水灌溉
      利用矿化度大于2g/L的咸水灌溉农田使作物得以生长发育的技术措施。在淡水资源短缺的干旱、半干旱地区,为了抗旱增产,许多国家,如突尼斯、意大利、美国、苏联等国,都有咸水灌溉的实践;中东,特别是北非一些国家在具有良好排水和淋洗条件的砂壤土上,用3~8g/L的咸水进行灌溉;有的国家还用稀释的海水灌溉。中国陕西、甘肃、河南、河北、宁夏等省、自治区,也有利用咸水灌溉的经验。
  
  咸水灌溉的主要作用,是增加土壤含水量,稀释土壤溶液浓度,使作物能够生长发育。干旱季节土壤含水量减少,尤其在盐渍化的土地上,随着土壤含水量减少,土壤溶液浓度易于增高,作物吸收困难,根系因失水而死亡。灌咸水后,不仅增加了土壤水分,而且由于咸水的浓度相对较低,降低了土壤溶液浓度,形成了适于作物吸收水分和养分的条件,因而有明显的增产效益。
  
  合理利用咸水灌溉的技术措施主要有:①要有排水条件,以免因灌咸水而引起土壤积盐。可利用雨季降雨或有淡水灌溉时,通过淋洗将盐分排出,使土壤周年不积盐;或在干旱年积盐,平水年及湿润年脱盐。②严格掌握水质标准。一般pH值为7~8,阴离子以硫酸根为主,阳离子中的钠不超过60%,矿化度一般不超过5g/L。③尽量减少灌水次数,宜在作物拔节以后,浇一二次关键水,且灌水定额不宜过大。④有淡水的地方,要咸淡轮灌或咸淡混灌,利用淡水洗盐。⑤加强农业措施,如平整土地,防止灌后局部高地返盐;增施有机肥,培肥地力,抑制返盐;灌后及时中耕锄土,减少土壤蒸发返盐;选种耐盐作物等。⑥若引起长时间连续积盐,应适当休闲,种植牧草,利用伏雨淋洗,或秋冬引淡水冲洗,脱盐后再改种一般作物。
  
  利用浅层地下咸水灌溉,还能降低地下水位,腾出地下调蓄库容,更有利于蓄纳雨水与非灌溉期的地表水,防治渍涝与盐碱灾害,促进地下水淡化。
  

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