内蒙古农业科技
內矇古農業科技
내몽고농업과기
INNER MONGOLIA AGRICULTURAL SCIENCE AND TECHNOLOGY
2015年
3期
72-74
,共3页
魏学%李超%张新龙%马睿妍%李俊有
魏學%李超%張新龍%馬睿妍%李俊有
위학%리초%장신룡%마예연%리준유
春播期%土壤墒情%气象条件%相关分析
春播期%土壤墑情%氣象條件%相關分析
춘파기%토양상정%기상조건%상관분석
Spring sowing period%Soil moisture%Meteorological conditions%Correlation analysis
利用内蒙古赤峰地区10个监测站2005-2014年的气象资料和春播期土壤墒情监测数据,分析了春播期土壤墒情与气象条件的关系。结果表明,赤峰地区10个监测站春播前降水量、日照时数、气温、风速与秋季对应气象要素值变化趋势一致,具有明显的差异性,而蒸发量之间无明显变化。从区域分布来看,南部地区土壤墒情好于北部地区。春播前和秋季降水量与土壤相对湿度相关系数分别为0.411和0.358,均达到极显著正相关(P<0.01),蒸发量与土壤相对湿度相关系数分别为-0.216*和-0.269*,均达到显著负相关(P<0.05),说明降水量对土壤墒情的提高具有明显的促进效应,蒸发量对土壤墒情的增加具有明显的抑制作用。
利用內矇古赤峰地區10箇鑑測站2005-2014年的氣象資料和春播期土壤墑情鑑測數據,分析瞭春播期土壤墑情與氣象條件的關繫。結果錶明,赤峰地區10箇鑑測站春播前降水量、日照時數、氣溫、風速與鞦季對應氣象要素值變化趨勢一緻,具有明顯的差異性,而蒸髮量之間無明顯變化。從區域分佈來看,南部地區土壤墑情好于北部地區。春播前和鞦季降水量與土壤相對濕度相關繫數分彆為0.411和0.358,均達到極顯著正相關(P<0.01),蒸髮量與土壤相對濕度相關繫數分彆為-0.216*和-0.269*,均達到顯著負相關(P<0.05),說明降水量對土壤墑情的提高具有明顯的促進效應,蒸髮量對土壤墑情的增加具有明顯的抑製作用。
이용내몽고적봉지구10개감측참2005-2014년적기상자료화춘파기토양상정감측수거,분석료춘파기토양상정여기상조건적관계。결과표명,적봉지구10개감측참춘파전강수량、일조시수、기온、풍속여추계대응기상요소치변화추세일치,구유명현적차이성,이증발량지간무명현변화。종구역분포래간,남부지구토양상정호우북부지구。춘파전화추계강수량여토양상대습도상관계수분별위0.411화0.358,균체도겁현저정상관(P<0.01),증발량여토양상대습도상관계수분별위-0.216*화-0.269*,균체도현저부상관(P<0.05),설명강수량대토양상정적제고구유명현적촉진효응,증발량대토양상정적증가구유명현적억제작용。
The relationship between soil moisture during spring sowing and meteorological conditions were comprehensively researched with the observed data related to soil moisture content and meteorological conditions during ten continual growing seasons from 2005 to 2014 in Chifeng.The results showed that the precipitation, sunshine, temperature, wind speed before spring sowing period and in autumn have the same dynamic changes, but evaporation has different dynamic changes.The regional distribution of soil moisture in south of Chifeng is better than in north of Chifeng.For five meteorological factors, precipitation very significantly positive correlated with relative soil moisture,and the simple correlation coefficients were 0.411,0.358,respectly before spring sowing period and in autumn,evaporation significantly negative correlated with relative soil moisture,and the simple correlation coefficients were-0.216,-0.269,which implied precipitation and evaporation were the most important factors in determining soil moisture in spring sowing period.