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微咸水矿化度对重度盐碱土壤入渗特征的影响

刘小媛 高佩玲 张晴雯 王乃江 赵连东

干旱地区农业研究2018,Vol.36Issue(1):102-107,6.
干旱地区农业研究2018,Vol.36Issue(1):102-107,6.DOI:10.7606/j.issn.1000-7601.2018.01.16

微咸水矿化度对重度盐碱土壤入渗特征的影响

Effect of mineralization degree of infiltration water on infiltration characteristics of severely saline-alkali soil

刘小媛 1高佩玲 1张晴雯 2王乃江 3赵连东1

作者信息

  • 1. 山东理工大学 农业工程与食品科学学院,山东 淄博255000
  • 2. 山东理工大学 资源与环境工程学院,山东 淄博255000
  • 3. 中国农业科学院农业环境与可持续发展研究所,北京100086
  • 折叠

摘要

Abstract

One-dimension vertical water infiltration experiments were conducted using a vertical soil column.The study was conducted to study the relations between cumulative infiltration,wetting front depth,soil moisture content,in-filtration rate and infiltration time under different mineralization degree of infiltration water.The results showed that cu-mulative infiltration,wetting front depth,soil moisture content increased with the mineralization degree of infiltration wa-ter.However,compared with fresh water,the changes of wetting front depth and cumulative infiltration of 2,3,4 g·L-1 and 5 g·L-1is smaller.In the same depth of soil,soil moisture content was characterized by fresh water <5 g·L-1<3 g·L-1<2 g·L-1<4 g·L-1.Cumulative infiltration was in good linear relationship with wetting front depth under brackish water irrigation.The Kostiakov infiltration model,Philip infiltration model and Green-Ampt infiltration model was compared in terms of quantifying saline water infiltration process,by which Kostiakov model was proposed.

关键词

微咸水/湿润锋/累积入渗量/土壤含水率/入渗率模型

Key words

brackish water/wetting front depth/cumulative infiltration/infiltration moisture content/infiltration model

分类

农业科技

引用本文复制引用

刘小媛,高佩玲,张晴雯,王乃江,赵连东..微咸水矿化度对重度盐碱土壤入渗特征的影响[J].干旱地区农业研究,2018,36(1):102-107,6.

基金项目

国家水体污染控制与治理科技重大专项(2015ZX07203-007) (2015ZX07203-007)

国家自然科学基金(41402208) (41402208)

山东省自然科学基金(ZR2011EL020) (ZR2011EL020)

国家级大学生创新创业训练计划项目(201510433047) (201510433047)

山东省自然科学基金项目(ZR2016EEM34) (ZR2016EEM34)

干旱地区农业研究

OACSCDCSTPCD

1000-7601

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