草业学报
草業學報
초업학보
PRATACULTURAL SCIENCE
2014年
6期
78-86
,共9页
陈骥%曹军骥%魏永林%刘吉宏%马扶林%陈迪超%冯嘉裕%夏瑶%岑燕
陳驥%曹軍驥%魏永林%劉吉宏%馬扶林%陳迪超%馮嘉裕%夏瑤%岑燕
진기%조군기%위영림%류길굉%마부림%진적초%풍가유%하요%잠연
青海湖流域%草甸草原%非生长季%土壤呼吸%土壤温度%土壤湿度
青海湖流域%草甸草原%非生長季%土壤呼吸%土壤溫度%土壤濕度
청해호류역%초전초원%비생장계%토양호흡%토양온도%토양습도
watershed of Qinghai Lake%meadow grassland%dormant season%soil respiration%soil temperature%soil moisture
非生长季土壤呼吸是生态系统碳循环的重要组成部分,显著地影响着碳收支。本研究利用 Li-8100开路式碳通量测定系统,研究了青海湖北岸高寒草甸草原非生长季土壤呼吸对短期围栏封育(自由放牧,3年围栏封育和5年围栏封育样地)的响应,并讨论了温度和湿度对非生长季土壤呼吸的影响。结果表明,1)自由放牧、3年围栏封育和5年围栏封育样地非生长季土壤呼吸平均速率分别是全年土壤呼吸平均速率的0.21,0.22和0.19倍;2)自由放牧、3年围栏封育和5年围栏封育样地非生长季土壤呼吸所排放的碳量分别为117.2,109.2和100.7 g C/m2,占全年土壤呼吸所排放的碳量的21.2%,22.3%和23.2%;3)相比于生长季和全年土壤呼吸的温度敏感性,非生长季具有更低的土壤呼吸温度敏感性;4)非生长季土壤温度和土壤湿度对土壤呼吸的解释率相当,一定的土壤湿度是保证土壤呼吸对温度响应的必要条件。因此,当考虑到碳收支和生态系统碳循环时不能忽略掉非生长季土壤呼吸的作用,而且水分在调节非生长季土壤呼吸中起着重要的作用。
非生長季土壤呼吸是生態繫統碳循環的重要組成部分,顯著地影響著碳收支。本研究利用 Li-8100開路式碳通量測定繫統,研究瞭青海湖北岸高寒草甸草原非生長季土壤呼吸對短期圍欄封育(自由放牧,3年圍欄封育和5年圍欄封育樣地)的響應,併討論瞭溫度和濕度對非生長季土壤呼吸的影響。結果錶明,1)自由放牧、3年圍欄封育和5年圍欄封育樣地非生長季土壤呼吸平均速率分彆是全年土壤呼吸平均速率的0.21,0.22和0.19倍;2)自由放牧、3年圍欄封育和5年圍欄封育樣地非生長季土壤呼吸所排放的碳量分彆為117.2,109.2和100.7 g C/m2,佔全年土壤呼吸所排放的碳量的21.2%,22.3%和23.2%;3)相比于生長季和全年土壤呼吸的溫度敏感性,非生長季具有更低的土壤呼吸溫度敏感性;4)非生長季土壤溫度和土壤濕度對土壤呼吸的解釋率相噹,一定的土壤濕度是保證土壤呼吸對溫度響應的必要條件。因此,噹攷慮到碳收支和生態繫統碳循環時不能忽略掉非生長季土壤呼吸的作用,而且水分在調節非生長季土壤呼吸中起著重要的作用。
비생장계토양호흡시생태계통탄순배적중요조성부분,현저지영향착탄수지。본연구이용 Li-8100개로식탄통량측정계통,연구료청해호북안고한초전초원비생장계토양호흡대단기위란봉육(자유방목,3년위란봉육화5년위란봉육양지)적향응,병토론료온도화습도대비생장계토양호흡적영향。결과표명,1)자유방목、3년위란봉육화5년위란봉육양지비생장계토양호흡평균속솔분별시전년토양호흡평균속솔적0.21,0.22화0.19배;2)자유방목、3년위란봉육화5년위란봉육양지비생장계토양호흡소배방적탄량분별위117.2,109.2화100.7 g C/m2,점전년토양호흡소배방적탄량적21.2%,22.3%화23.2%;3)상비우생장계화전년토양호흡적온도민감성,비생장계구유경저적토양호흡온도민감성;4)비생장계토양온도화토양습도대토양호흡적해석솔상당,일정적토양습도시보증토양호흡대온도향응적필요조건。인차,당고필도탄수지화생태계통탄순배시불능홀략도비생장계토양호흡적작용,이차수분재조절비생장계토양호흡중기착중요적작용。
Dormant season soil CO2 efflux is a significant component of the ecosystem carbon cycle and it there-fore plays an important role in carbon budgets calculated to address global climate change.This study investi-gates the response of dormant season soil CO2 efflux to short-term grazing exclusion.It also explores the im-pacts of soil temperature and moisture on soil respiration using the Li-8100 system.Soil respiration was studied in three blocks-free-range grazing (FG),grazing exclusion for 3 years (GE3 ),and grazing exclusion for 5 years (GE5 ).Respectively,the average dormant season soil respiration was 0.21,0.22,and 0.19 times of the annu-al average soil respiration in each of the three blocks.The carbon released by soil respiration during the dor-mant season was 117.2,109.2 and 100.7 g/cm2 ,accounted for 21.2%,22.3% and 23.2% of the amount of annual carbon released from soil for FG,GE3 and GE5 ,respectively.The Q10 values during the dormant season were lower than both the annual and growing season scores.Soil temperature and moisture almost equally ac-count for the variation in soil respiration,and a certain amount of soil water content is necessary for maintai-ning the response of soil respiration to soil temperature.Therefore,when considering the carbon budget and cycle of ecosystems,we cannot ignore dormant season soil respiration;and soil moisture plays a considerable role in regulating this process.