东北林业大学学报
東北林業大學學報
동북임업대학학보
JOURNAL OF NORTHEAST FORESTRY UNIVERSITY
2009年
11期
82-83,95
,共3页
徐庆华%刘勇%马履一%王少华%侯炳柱%尹凤君
徐慶華%劉勇%馬履一%王少華%侯炳柱%尹鳳君
서경화%류용%마리일%왕소화%후병주%윤봉군
黑土%蒸发量%土壤含水量%气象因子
黑土%蒸髮量%土壤含水量%氣象因子
흑토%증발량%토양함수량%기상인자
Arable mollisol%Evaporation%Soil moisture%Meteorological factors
为准确地掌握东北农田黑土水分蒸发量的变化规律,2007年8月开始在吉林省吉林市龙潭区江密峰苗圃进行蒸发量测量试验,采用称质量法测量不同设置水分条件下农田黑土的昼夜蒸发量,并根据蒸发量与测量的气象因子建立了相应的回归方程.结果表明:土壤蒸发量与土壤含水量呈极显著正相关;土壤蒸发量在不同土壤含水量之间差异显著.通常情况下,土壤白天的蒸发量大约是夜间的12倍,全天蒸发量集中在11:00-15:00,占全天蒸发量的60%~70%.土壤蒸发量与光合有效辐射和风速呈显著的正相关,与其它气象因子相关关系不显著.
為準確地掌握東北農田黑土水分蒸髮量的變化規律,2007年8月開始在吉林省吉林市龍潭區江密峰苗圃進行蒸髮量測量試驗,採用稱質量法測量不同設置水分條件下農田黑土的晝夜蒸髮量,併根據蒸髮量與測量的氣象因子建立瞭相應的迴歸方程.結果錶明:土壤蒸髮量與土壤含水量呈極顯著正相關;土壤蒸髮量在不同土壤含水量之間差異顯著.通常情況下,土壤白天的蒸髮量大約是夜間的12倍,全天蒸髮量集中在11:00-15:00,佔全天蒸髮量的60%~70%.土壤蒸髮量與光閤有效輻射和風速呈顯著的正相關,與其它氣象因子相關關繫不顯著.
위준학지장악동북농전흑토수분증발량적변화규률,2007년8월개시재길림성길림시룡담구강밀봉묘포진행증발량측량시험,채용칭질량법측량불동설치수분조건하농전흑토적주야증발량,병근거증발량여측량적기상인자건립료상응적회귀방정.결과표명:토양증발량여토양함수량정겁현저정상관;토양증발량재불동토양함수량지간차이현저.통상정황하,토양백천적증발량대약시야간적12배,전천증발량집중재11:00-15:00,점전천증발량적60%~70%.토양증발량여광합유효복사화풍속정현저적정상관,여기타기상인자상관관계불현저.
An evaporation experiment was conducted to study the daily variation of evaporation on arable mollisol under different soil moisture conditions in Jiangmifeng Nursery of Longtan District, Jilin City in October 2007. Regressive equations be-tween evaporation on arable mollisol and meteorological factors were established in terms of the evaporation for both day and night under different soil moisture conditions. Results showed that evaporation was positively correlated with soil moisture,and there was a significant difference in evaporation between different soil moisture levels. The evaporation for day was u-sually 12 times as much as that for night, and the peak of evaporation occurred between 11am and 15 pm, accounting for 60% ~70% of the total. The evaporation of arable mollisol was positively related to photosynthetically active radiation and wind speed, but insignificantly related to other meteorological factors.