湖北农业科学
湖北農業科學
호북농업과학
2009年
11期
2706-2711
,共6页
李洪波%白爱宁%张国盛%王林和%杨新林%张瑜
李洪波%白愛寧%張國盛%王林和%楊新林%張瑜
리홍파%백애저%장국성%왕림화%양신림%장유
臭柏冠层%凝结水%形成和作用%内蒙古半干旱区
臭柏冠層%凝結水%形成和作用%內矇古半榦旱區
취백관층%응결수%형성화작용%내몽고반간한구
canopy of Sabina vulgaris%dew%formation and effect%semi-arid area in Inner Mongolia
为探讨凝结水对臭柏的作用,采用人造凝结面法、离体枝条法和盆栽封袋法,分析了在干旱季节臭柏冠层凝结水的形成和作用.结果表明,臭柏冠层凝结能力从大到小依次为100、50、150和5cm,其中100cm处凝结时间最长,能够代表冠层拦截凝结水的能力,该处凝结水的发生分为3个阶段,即发生前期(14:00~22:00)、发生时段(22:00至次日8:00)和蒸发时段(8:00~14:00).人造凝结面和离体枝条凝结水拦截量都与凝结持续时间呈线性正相关.高密度栽植的臭柏冠层可以不间断地向土壤方向输入水汽.通过盆栽封袋法证明凝结水对臭柏作用显著.
為探討凝結水對臭柏的作用,採用人造凝結麵法、離體枝條法和盆栽封袋法,分析瞭在榦旱季節臭柏冠層凝結水的形成和作用.結果錶明,臭柏冠層凝結能力從大到小依次為100、50、150和5cm,其中100cm處凝結時間最長,能夠代錶冠層攔截凝結水的能力,該處凝結水的髮生分為3箇階段,即髮生前期(14:00~22:00)、髮生時段(22:00至次日8:00)和蒸髮時段(8:00~14:00).人造凝結麵和離體枝條凝結水攔截量都與凝結持續時間呈線性正相關.高密度栽植的臭柏冠層可以不間斷地嚮土壤方嚮輸入水汽.通過盆栽封袋法證明凝結水對臭柏作用顯著.
위탐토응결수대취백적작용,채용인조응결면법、리체지조법화분재봉대법,분석료재간한계절취백관층응결수적형성화작용.결과표명,취백관층응결능력종대도소의차위100、50、150화5cm,기중100cm처응결시간최장,능구대표관층란절응결수적능력,해처응결수적발생분위3개계단,즉발생전기(14:00~22:00)、발생시단(22:00지차일8:00)화증발시단(8:00~14:00).인조응결면화리체지조응결수란절량도여응결지속시간정선성정상관.고밀도재식적취백관층가이불간단지향토양방향수입수기.통과분재봉대법증명응결수대취백작용현저.
For researching of the effect of dew on Sabina vulgaris,using methods of artificial condensation surface,detached shoots and bag closure of petted culture to determine dew formation and absorption by canopy of Sabina vulgaris on arid season.The results indicated that the capacity of dew formation was the biggest on 100cm of Sabina vulgaris canopy,which can represent capacity of the whole canopy.There were three periods that were the previous period of dew formation(14:00~22:0),the period of dew formation(22:00~8:00),the evapemted period of dew(8:00~14:00),respectively.The intercepting quantity of dew by artificial condensation surface and detached shoots were linear positive correlation with dew duration.Sabina vulgaris canopy of high density could uninterrupted provide water vapor to soil direction,at the sanle time,effect of dew wag significant to Sabina vulgaris.