Effect of Near-Earth Surface Temperature on Soil Temperature at 5 cm Depth

O. Adebayo, Y. B. Lawal, O. R. Obasi-Oma, John Sunday Ojo
{"title":"Effect of Near-Earth Surface Temperature on Soil Temperature at 5 cm Depth","authors":"O. Adebayo, Y. B. Lawal, O. R. Obasi-Oma, John Sunday Ojo","doi":"10.9734/psij/2022/v26i330316","DOIUrl":null,"url":null,"abstract":"The research investigates the effects of ground surface temperature (air temperature) on soil temperature at a depth of 5 cm. The study covers a period of fourteen (14) months from May 2010 to June 2011 in Akure, Southwestern Nigeria. With the aid of an automatic weather station, temperature readings were taken at a depth of 5 cm below the soil surface at five (5) minute intervals daily. It was also observed that many analyses of soil temperature are based on the theories of heat flow and energy balance. The study reveals that surface temperature has a weak effect on soil temperature. The best correlation coefficient obtained for the study period is about 0.56 with a quadratic equation of order 2 at 5% significance level. This implies that air temperature cannot be solely used to predict soil temperature at a depth of 5 cm. A study of diurnal variation reveals that air temperature is usually higher than soil temperature during the day, and vice versa. The study also revealed that surface and soil temperatures are generally lower during the wet months when compared with the dry months. The wet season average daily temperatures are 23.42oC and 27.69oC for air and soil while the corresponding dry season values are 33.92oC and 30.91oC respectively. The results are recommended for agricultural purposes such as determination of soil and environmental conditions for crop production.","PeriodicalId":124795,"journal":{"name":"Physical Science International Journal","volume":"28 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-08-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Physical Science International Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.9734/psij/2022/v26i330316","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0

Abstract

The research investigates the effects of ground surface temperature (air temperature) on soil temperature at a depth of 5 cm. The study covers a period of fourteen (14) months from May 2010 to June 2011 in Akure, Southwestern Nigeria. With the aid of an automatic weather station, temperature readings were taken at a depth of 5 cm below the soil surface at five (5) minute intervals daily. It was also observed that many analyses of soil temperature are based on the theories of heat flow and energy balance. The study reveals that surface temperature has a weak effect on soil temperature. The best correlation coefficient obtained for the study period is about 0.56 with a quadratic equation of order 2 at 5% significance level. This implies that air temperature cannot be solely used to predict soil temperature at a depth of 5 cm. A study of diurnal variation reveals that air temperature is usually higher than soil temperature during the day, and vice versa. The study also revealed that surface and soil temperatures are generally lower during the wet months when compared with the dry months. The wet season average daily temperatures are 23.42oC and 27.69oC for air and soil while the corresponding dry season values are 33.92oC and 30.91oC respectively. The results are recommended for agricultural purposes such as determination of soil and environmental conditions for crop production.
近地表面温度对5 cm深度土壤温度的影响
本研究考察了地表温度(空气温度)对5厘米深度土壤温度的影响。该研究在尼日利亚西南部的阿库雷进行,为期14个月,从2010年5月到2011年6月。在自动气象站的帮助下,每天每隔5分钟在土壤表面以下5厘米的深度采集温度数据。人们还注意到,许多土壤温度分析是基于热流理论和能量平衡理论。研究表明,地表温度对土壤温度的影响较小。研究期间的最佳相关系数约为0.56,在5%显著性水平下为2阶二次方程。这意味着空气温度不能单独用来预测5厘米深的土壤温度。对日变化的研究表明,白天气温通常高于土壤温度,反之亦然。该研究还表明,与干旱月份相比,潮湿月份的地表和土壤温度通常较低。湿季空气和土壤日平均气温分别为23.42oC和27.69oC,干季分别为33.92oC和30.91oC。该结果推荐用于农业用途,如测定作物生产的土壤和环境条件。
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