生态环境学报
生態環境學報
생태배경학보
Ecology and Environment Sciences
2015年
9期
1453-1460
,共8页
李吉玫%张毓涛%韩燕梁%李翔
李吉玫%張毓濤%韓燕樑%李翔
리길매%장육도%한연량%리상
降水变化%天山云杉%细根分解%养分释放%干旱区山地森林
降水變化%天山雲杉%細根分解%養分釋放%榦旱區山地森林
강수변화%천산운삼%세근분해%양분석방%간한구산지삼림
precipitation%Picea schrenkiana var.tianshanica%fine root decomposition%nutrient release%arid mountain fores
采用野外模拟试验,通过设计3种降水变化处理[ZP(去除降水)、CK(自然降水,对照)、DP(双倍降水)],研究了降水变化对天山云杉细根分解的影响。研究结果表明,分解24个月CK处理的细根干质量残留率分别是ZP和DP处理的80%和128%倍。除在分解进行到第8个月时,3种处理细根质量残留率差异不显著外(P>0.05),其余分解时期差异均显著(P<0.05)。3种处理下细根分解系数为DP(0.30)>CK(0.22)>ZP(0.08)。与CK处理下细根分解50%和95%的时间相比, ZP处理分别增加了5.47年和23.75年,DP处理分别减少了0.44年和1.91年,说明增加降水促进了天山云杉细根分解,而去除降水抑制了分解。CK和DP处理下细根月分解率表现为双峰型曲线,ZP处理则变化相对平稳的曲线。降水处理改变了细根分解过程中纤维素和木质素分解模式及N元素的释放模式,但对C元素的释放模式没有影响。
採用野外模擬試驗,通過設計3種降水變化處理[ZP(去除降水)、CK(自然降水,對照)、DP(雙倍降水)],研究瞭降水變化對天山雲杉細根分解的影響。研究結果錶明,分解24箇月CK處理的細根榦質量殘留率分彆是ZP和DP處理的80%和128%倍。除在分解進行到第8箇月時,3種處理細根質量殘留率差異不顯著外(P>0.05),其餘分解時期差異均顯著(P<0.05)。3種處理下細根分解繫數為DP(0.30)>CK(0.22)>ZP(0.08)。與CK處理下細根分解50%和95%的時間相比, ZP處理分彆增加瞭5.47年和23.75年,DP處理分彆減少瞭0.44年和1.91年,說明增加降水促進瞭天山雲杉細根分解,而去除降水抑製瞭分解。CK和DP處理下細根月分解率錶現為雙峰型麯線,ZP處理則變化相對平穩的麯線。降水處理改變瞭細根分解過程中纖維素和木質素分解模式及N元素的釋放模式,但對C元素的釋放模式沒有影響。
채용야외모의시험,통과설계3충강수변화처리[ZP(거제강수)、CK(자연강수,대조)、DP(쌍배강수)],연구료강수변화대천산운삼세근분해적영향。연구결과표명,분해24개월CK처리적세근간질량잔류솔분별시ZP화DP처리적80%화128%배。제재분해진행도제8개월시,3충처리세근질량잔류솔차이불현저외(P>0.05),기여분해시기차이균현저(P<0.05)。3충처리하세근분해계수위DP(0.30)>CK(0.22)>ZP(0.08)。여CK처리하세근분해50%화95%적시간상비, ZP처리분별증가료5.47년화23.75년,DP처리분별감소료0.44년화1.91년,설명증가강수촉진료천산운삼세근분해,이거제강수억제료분해。CK화DP처리하세근월분해솔표현위쌍봉형곡선,ZP처리칙변화상대평은적곡선。강수처리개변료세근분해과정중섬유소화목질소분해모식급N원소적석방모식,단대C원소적석방모식몰유영향。
A field simulated experiment was conducted to study the effects of variation of precipitation on the fine root decomposition and related nutrient release in Picea schrenkiana var.tianshanica. Three precipitation treatments were designed as ZP (zero precipitation), CK (natural precipitation, control) and DP (double precipitation). The results showed that, (1) After 24 months decomposition, the fine root remain percentage in CK of Picea schrenkiana var.tianshanica is 0.80 times in ZP and 1.28 times in DP. The differences of fine root remain percentage under three precipitation treatments in the eighth month since beginning decomposition were not significant (P>0.05), while the difference were significant in other decomposition stages (P<0.05). The fine root decomposition coefficient was DP (0.30)>CK (0.22)>ZP (0.08). Compared with the required times for fine root decomposition 50%and 95%in CK, they were longer than 5.45a and 23.75a in ZP treatment, and shorter than 0.44a and 1.91a. The results indicated that increase precipitation promoted the fine root decomposition, while removal precipitation inhibited its decomposition. (2)The fine root monthly decomposition rate in CK and DP were double peak curves, while it was relatively smooth curve in ZP. And (3) precipitation treatment changed the decomposition model of lignin and cellulose of Picea schrenkiana fine root decomposition and release model of N element, but it did not change release model of C element.