草原与草坪
草原與草坪
초원여초평
GRASSLAND AND TURF
2012年
3期
70-73
,共4页
邹雨坤%王丽%张静妮%陈秀蓉%杨殿林
鄒雨坤%王麗%張靜妮%陳秀蓉%楊殿林
추우곤%왕려%장정니%진수용%양전림
羊草草原%利用方式%碳矿化
羊草草原%利用方式%碳礦化
양초초원%이용방식%탄광화
Leymus chinensis%land use patterns%carbon mineralization
以内蒙古呼伦贝尔羊草草原为研究对象,利用室内培养法比较研究了刈割、放牧和围栏封育3种利用方式对羊草草原土壤碳矿化潜力的影响。结果表明:不同利用方式下,土壤碳矿化潜力不同。在25℃条件下,羊草草原0~10cm土层培养30d结束时的矿化速率在刈割、放牧和围封干扰下分别为培养开始5d时的15.3%,9.5%和10.2%;10~20cm土层培养30d结束时的矿化速率在刈割、放牧和围封干扰下分别为培养5d开始时的5.6%,18.6%和13.9%。0~10cm土层矿化累积释放的CO2-C量大小依次为刈割〉围封〉放牧,刈割与放牧样地差异显著。样地10~20cm土层矿化累积释放的CO2-C量大小依次为刈割〉放牧〉围封,刈割与围封样地差异显著,且0~10cm土层的CO2-C累积释放量〉10~20cm土层。
以內矇古呼倫貝爾羊草草原為研究對象,利用室內培養法比較研究瞭刈割、放牧和圍欄封育3種利用方式對羊草草原土壤碳礦化潛力的影響。結果錶明:不同利用方式下,土壤碳礦化潛力不同。在25℃條件下,羊草草原0~10cm土層培養30d結束時的礦化速率在刈割、放牧和圍封榦擾下分彆為培養開始5d時的15.3%,9.5%和10.2%;10~20cm土層培養30d結束時的礦化速率在刈割、放牧和圍封榦擾下分彆為培養5d開始時的5.6%,18.6%和13.9%。0~10cm土層礦化纍積釋放的CO2-C量大小依次為刈割〉圍封〉放牧,刈割與放牧樣地差異顯著。樣地10~20cm土層礦化纍積釋放的CO2-C量大小依次為刈割〉放牧〉圍封,刈割與圍封樣地差異顯著,且0~10cm土層的CO2-C纍積釋放量〉10~20cm土層。
이내몽고호륜패이양초초원위연구대상,이용실내배양법비교연구료예할、방목화위란봉육3충이용방식대양초초원토양탄광화잠력적영향。결과표명:불동이용방식하,토양탄광화잠력불동。재25℃조건하,양초초원0~10cm토층배양30d결속시적광화속솔재예할、방목화위봉간우하분별위배양개시5d시적15.3%,9.5%화10.2%;10~20cm토층배양30d결속시적광화속솔재예할、방목화위봉간우하분별위배양5d개시시적5.6%,18.6%화13.9%。0~10cm토층광화루적석방적CO2-C량대소의차위예할〉위봉〉방목,예할여방목양지차이현저。양지10~20cm토층광화루적석방적CO2-C량대소의차위예할〉방목〉위봉,예할여위봉양지차이현저,차0~10cm토층적CO2-C루적석방량〉10~20cm토층。
Carbon mineralization potential of mowed,grazed and fenced Leymus chinensis steppes was determined in Hulunbeier grassland of Inner Mongolia by using approaches of culture under lab condition. The results showed that carbon mineralization potential was different under different land use patterns. The velocity of carbon mineralization at 5 d was 15.3%,9.5% and 10.2% respectively in layer of 0-10 cm,and 5.6%,18.6% and 13.9% respectively at 5 d in layer of 10-20 cm. The content of CO2-C released from the mineralization of soil organic C can be ordered as mowing plots〉fencing plots〉grazing plots in layer of 0-10 cm;and mowing plots〉grazing plots〉fencing plots in layer of 10-20 cm. The total content of CO2-C released from the mineralization of soil organic C in layer of 0-10 cm was higher than the layer of 10-20 cm.