北方环境
北方環境
북방배경
INNER MONGOLIA ENVIRONMENTAL SCIENCES
2013年
11期
43-46
,共4页
科尔沁沙地%叶凋落物%土壤含水量%沙漠化
科爾沁沙地%葉凋落物%土壤含水量%沙漠化
과이심사지%협조락물%토양함수량%사막화
Horqin sandy land%leaf litters%soil water content%desertification
采用可以有效控制环境因子的室内土壤培养试验,对固定沙地土壤不同水分作用下叶凋落物释放CO2的情况进行了初步研究。结果表明:土壤CO2的释放量及凋落物的分解均与土壤干湿情况相关。在添加凋落物与不添加凋落物的处理中,培养前4天的低含水条件下CO2释放速率与中高含水处理相比差异均呈极显著,而4天以后不同水分条件下的释放速率无显著差异。在沙地中,土壤过于湿润或干旱均能够阻碍凋落物的分解。
採用可以有效控製環境因子的室內土壤培養試驗,對固定沙地土壤不同水分作用下葉凋落物釋放CO2的情況進行瞭初步研究。結果錶明:土壤CO2的釋放量及凋落物的分解均與土壤榦濕情況相關。在添加凋落物與不添加凋落物的處理中,培養前4天的低含水條件下CO2釋放速率與中高含水處理相比差異均呈極顯著,而4天以後不同水分條件下的釋放速率無顯著差異。在沙地中,土壤過于濕潤或榦旱均能夠阻礙凋落物的分解。
채용가이유효공제배경인자적실내토양배양시험,대고정사지토양불동수분작용하협조락물석방CO2적정황진행료초보연구。결과표명:토양CO2적석방량급조락물적분해균여토양간습정황상관。재첨가조락물여불첨가조락물적처리중,배양전4천적저함수조건하CO2석방속솔여중고함수처리상비차이균정겁현저,이4천이후불동수분조건하적석방속솔무현저차이。재사지중,토양과우습윤혹간한균능구조애조락물적분해。
This experiment uses laboratory soil incubation experiment that can control environment factor measures the effect on CO 2 re-lease of leaf litters in different water content in fixed dunes .The results showed that:Total CO2 release and litter decomposition were corre-lated to water content of soil .Whether litter added or not , CO2 release rate of low water content was significantly different from that of medi -um and high water contents in the first 4 days.In sand land, either wetness or dryness of soil imposed great influence on litter decomposi -tion, because soil and litter CO2 release amount were significantly different from that of the water content .