Management of saline and sodic soils

P. Ramamoorthy, M. Karthikeyan, V. Nirubana
{"title":"Management of saline and sodic soils","authors":"P. Ramamoorthy, M. Karthikeyan, V. Nirubana","doi":"10.51483/IJAGST.1.1.2021.24-27","DOIUrl":null,"url":null,"abstract":"Saline and sodic (alkali) soils can significantly reduce the value and productivity of affected land. Soil salinity and related problems generally occur in arid or semiarid climates where rainfall is insufficient to leach soluble salts from the soil or where surface or internal soil drainage is restricted. Salinity problems can also occur on irrigated land, particularly when irrigation water quality is marginal or worse. It has been estimated that slightly more than one-fourth of irrigated farmland in the United States is affected by soil salinity. In humid regions salt problems are less likely because rainfall is sufficient to leach soluble salts from the soil, but even in higher rainfall areas, salinity problems occur. In some areas with high water tables, problems may occur with surface evaporation leaving salts to accumulate. In Kansas, salt-affected soils and related problems occur statewide but often on small areas. Field-wide problems often are due to poor quality irrigation water and/or excessive manure applications. Drilling activity causing high-salt water to escape to the soil surface, spills, or natural causes may result in spotty problems. Some areas of the state where salt mining occurs, particularly south central Kansas, have soils naturally high in sodium and soluble salts. Ions most commonly associated with soil salinity include the anions chloride (Cl-), sulfate (SO4), carbonate (HCO3), and sometimes nitrate (NO3) and the cations sodium (Na+), calcium (Ca++), magnesium (Mg++), and sometimes potassium (K+). Salts of these ions occur in highly variable concentrations and proportions. Saltaffected soils have been called white alkali, black alkali, gumbo, slick spots and other descriptive names. These names are associated with soil appearances caused by salt accumulation. The term alkali often refers to soils light in color and prone to surface crusting and implies that affected soils are high in exchangeable sodium. Salt-affected soils differ considerably in use suitability, productivity, ease of reclamation, and management.","PeriodicalId":122886,"journal":{"name":"International Journal of Agricultural Sciences and Technology","volume":"46 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2021-02-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"11","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal of Agricultural Sciences and Technology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.51483/IJAGST.1.1.2021.24-27","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 11

Abstract

Saline and sodic (alkali) soils can significantly reduce the value and productivity of affected land. Soil salinity and related problems generally occur in arid or semiarid climates where rainfall is insufficient to leach soluble salts from the soil or where surface or internal soil drainage is restricted. Salinity problems can also occur on irrigated land, particularly when irrigation water quality is marginal or worse. It has been estimated that slightly more than one-fourth of irrigated farmland in the United States is affected by soil salinity. In humid regions salt problems are less likely because rainfall is sufficient to leach soluble salts from the soil, but even in higher rainfall areas, salinity problems occur. In some areas with high water tables, problems may occur with surface evaporation leaving salts to accumulate. In Kansas, salt-affected soils and related problems occur statewide but often on small areas. Field-wide problems often are due to poor quality irrigation water and/or excessive manure applications. Drilling activity causing high-salt water to escape to the soil surface, spills, or natural causes may result in spotty problems. Some areas of the state where salt mining occurs, particularly south central Kansas, have soils naturally high in sodium and soluble salts. Ions most commonly associated with soil salinity include the anions chloride (Cl-), sulfate (SO4), carbonate (HCO3), and sometimes nitrate (NO3) and the cations sodium (Na+), calcium (Ca++), magnesium (Mg++), and sometimes potassium (K+). Salts of these ions occur in highly variable concentrations and proportions. Saltaffected soils have been called white alkali, black alkali, gumbo, slick spots and other descriptive names. These names are associated with soil appearances caused by salt accumulation. The term alkali often refers to soils light in color and prone to surface crusting and implies that affected soils are high in exchangeable sodium. Salt-affected soils differ considerably in use suitability, productivity, ease of reclamation, and management.
盐碱地和盐碱地的管理
盐碱土和钠(碱)土会显著降低受影响土地的价值和生产力。土壤盐碱化和相关问题一般发生在干旱或半干旱气候中,在这些地区,降雨量不足以从土壤中滤出可溶性盐,或地表或内部土壤排水受到限制。盐碱化问题也可能发生在灌溉土地上,特别是在灌溉水质较差或较差的情况下。据估计,美国略多于四分之一的灌溉农田受到土壤盐碱化的影响。在潮湿地区,盐问题不太可能发生,因为降雨足以从土壤中滤出可溶性盐,但即使在降雨较多的地区,盐问题也会发生。在一些地下水位高的地区,可能会出现地表蒸发导致盐积累的问题。在堪萨斯州,盐渍土壤和相关问题在全州范围内都有发生,但通常发生在小区域。整个农田的问题往往是由于灌溉水质量差和/或施用过多肥料造成的。钻井活动导致高盐水泄漏到土壤表面,泄漏或自然原因可能导致斑点问题。堪萨斯州的一些盐矿开采地区,特别是堪萨斯州的中南部,土壤中钠和可溶性盐的天然含量很高。与土壤盐度最相关的离子包括阴离子氯离子(Cl-)、硫酸盐离子(SO4)、碳酸盐离子(HCO3),有时还有硝酸盐离子(NO3)和阳离子钠离子(Na+)、钙离子(Ca++)、镁离子(Mg++),有时还有钾离子(K+)。这些离子的盐的浓度和比例变化很大。盐渍土壤被称为白碱、黑碱、秋葵、油渍和其他描述性名称。这些名称与盐积累引起的土壤外观有关。碱性一词通常是指颜色较浅、表面容易结壳的土壤,暗示受影响的土壤交换性钠含量高。受盐渍影响的土壤在使用适宜性、生产力、复垦难易程度和管理方面差别很大。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信