{"title":"Bowen ratio and evapotranspiration dynamics of oil palm","authors":"Muhammad Fajar Asyura, T. June, Resti Salmayenti","doi":"10.13057/tropdrylands/t070105","DOIUrl":null,"url":null,"abstract":"Abstract. Asyura MF, June T, Salmayenti R. 2023. Bowen ratio and evapotranspiration dynamics of oil palm. Intl J Trop Drylands 7: 37-45. To optimize its biophysical processes, plant needs water and this requirement can be quantified as Evapotranspiration (ET). There are various methods for estimating ET from a vegetated surface, and Bowen ratio is one method commonly used for agricultural purposes. We use Bowen ratio method to estimate ET from oil palm (Elaeis guineensis Jacq.) plantation in PT. Perkebunan Nusantara VI, Batang Hari, Jambi Province, Indonesia for the period 2014-2015 using observed micrometeorology data and looked at the strength of micrometeorological components in influencing the daily and diurnal patterns, which include net radiation (Rnetto), heat fluxes (latent LE and sensible H), actual vapor pressure (ea), soil moisture (SM), wind speed (WS), air temperature (Ta), ground heat fluxes (G), and LE-H. We found that the daily pattern of Bowen ratio was strongly influenced by LE-H, LE, H, SM, shown by a correlation coefficient of -0.85, -0.75, 0.84, -0.58, respectively. The diurnal pattern of Bowen ratio was affected by ea with a correlation coefficient of -0.52, while daily ET was strongly influenced by Rnetto, LE-H, H, Bowen ratio with a correlation coefficient of 0.85, 0.95, -0.63, -0.75 respectively. WS, Ta, Rnetto, G, ea, RH and LE-H affected diurnal ET with a correlation coefficient of 0.72, 0.72, 0.96, 0.89, 0.51, -0.64 and 0.9, respectively. Within this period of 2014-2015 there were 7 months where rainfall was greater than ET (wet period December 2014 to April 2015, November 2015) and 5 months where rainfall was lower than ET (dry period May 2015 to October 2015). During this long dry period of 2015, caused by strong El Nino events, oil palms became vulnerable to drought.","PeriodicalId":353102,"journal":{"name":"International Journal of Tropical Drylands","volume":"22 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-03-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"International Journal of Tropical Drylands","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.13057/tropdrylands/t070105","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
Abstract. Asyura MF, June T, Salmayenti R. 2023. Bowen ratio and evapotranspiration dynamics of oil palm. Intl J Trop Drylands 7: 37-45. To optimize its biophysical processes, plant needs water and this requirement can be quantified as Evapotranspiration (ET). There are various methods for estimating ET from a vegetated surface, and Bowen ratio is one method commonly used for agricultural purposes. We use Bowen ratio method to estimate ET from oil palm (Elaeis guineensis Jacq.) plantation in PT. Perkebunan Nusantara VI, Batang Hari, Jambi Province, Indonesia for the period 2014-2015 using observed micrometeorology data and looked at the strength of micrometeorological components in influencing the daily and diurnal patterns, which include net radiation (Rnetto), heat fluxes (latent LE and sensible H), actual vapor pressure (ea), soil moisture (SM), wind speed (WS), air temperature (Ta), ground heat fluxes (G), and LE-H. We found that the daily pattern of Bowen ratio was strongly influenced by LE-H, LE, H, SM, shown by a correlation coefficient of -0.85, -0.75, 0.84, -0.58, respectively. The diurnal pattern of Bowen ratio was affected by ea with a correlation coefficient of -0.52, while daily ET was strongly influenced by Rnetto, LE-H, H, Bowen ratio with a correlation coefficient of 0.85, 0.95, -0.63, -0.75 respectively. WS, Ta, Rnetto, G, ea, RH and LE-H affected diurnal ET with a correlation coefficient of 0.72, 0.72, 0.96, 0.89, 0.51, -0.64 and 0.9, respectively. Within this period of 2014-2015 there were 7 months where rainfall was greater than ET (wet period December 2014 to April 2015, November 2015) and 5 months where rainfall was lower than ET (dry period May 2015 to October 2015). During this long dry period of 2015, caused by strong El Nino events, oil palms became vulnerable to drought.
摘要刘建军,刘建军,刘建军,等。油棕的博文比与蒸散动态。《热带旱地》7:37 -45。为了优化其生物物理过程,植物需要水分,这种需要量可以量化为蒸散发(Evapotranspiration, ET)。从植被表面估算ET有多种方法,鲍文比是一种通常用于农业目的的方法。利用微气象观测资料,利用Bowen比值法估算了2014-2015年印尼占比省Batang Hari Perkebunan Nusantara VI PT油棕人工林的ET,并研究了影响日、日模式的微气象分量强度,包括净辐射(Rnetto)、热通量(潜热通量和感热通量)、实际蒸气压(ea)、土壤湿度(SM)、风速(WS)、气温(Ta)。地热通量(G),和LE-H。结果表明,波温比的日变化规律受LE-H、LE、H、SM的影响较大,相关系数分别为-0.85、-0.75、0.84、-0.58。波温比的日变化受ea的影响,相关系数为-0.52;日蒸散发受Rnetto、LE-H、H、波温比的影响较大,相关系数分别为0.85、0.95、-0.63、-0.75。WS、Ta、Rnetto、G、ea、RH和LE-H对日蒸散发的影响相关系数分别为0.72、0.72、0.96、0.89、0.51、-0.64和0.9。在2014-2015年期间,降雨量大于ET的有7个月(2014年12月至2015年4月,2015年11月),降雨量低于ET的有5个月(2015年5月至2015年10月)。在2015年这段由强厄尔尼诺事件造成的漫长干旱时期,油棕变得容易受到干旱的影响。