生态环境学报
生態環境學報
생태배경학보
ECOLOGY AND ENVIRONMENT
2015年
7期
1143-1149
,共7页
刘辉%杨万勤%倪祥银%肖洒%吴福忠
劉輝%楊萬勤%倪祥銀%肖灑%吳福忠
류휘%양만근%예상은%초쇄%오복충
高山森林%粗木质残体%腐烂等级%腐殖化
高山森林%粗木質殘體%腐爛等級%腐殖化
고산삼림%조목질잔체%부란등급%부식화
alpine forest%coarse woody debris%decay class%humification
高山森林粗木质残体腐殖化是促进生态系统土壤发育和碳吸存的主要途径之一,并可能受到腐烂等级和木质残体类型的影响,但一直缺乏必要的关注。因此,在2013年8月,以青藏高原东缘海拔3600 m左右的高山森林中具有代表性的岷江冷杉(Abies faxoniana)原始林为研究对象,根据区域内坡度和物种组成设置3个100 m×100 m的典型样地,在研究样地内随机选取5个腐烂等级的岷江冷杉粗木质残体,每个腐烂等级3株,4种粗木质残体,共计60株,调查和研究区域内不同腐烂等级倒木、枯立木、根桩和大枯枝等主要类型粗木质残体的腐殖化特征。结果表明:枯立木、大枯枝和倒木腐殖质碳、胡敏酸碳和富里酸碳含量随腐烂等级增加而增大,而根桩腐殖质碳、胡敏酸碳和富里酸碳含量随腐烂等级增加而减小,并且枯立木在各个分解阶段腐殖质碳、胡敏酸碳和富里酸碳含量均保持较高水平。同时,枯立木、大枯枝和倒木的腐殖化度随腐烂等级增加呈增大趋势,根桩腐殖化度却随着腐烂等级增加而减小,其腐殖化度分别为52.93%~85.88%、49.2%~73.68%、54.94%~67.21%和53.41%~68.68%。枯立木腐殖化度明显高于其他3种类型粗木质残体,且在腐殖化后期(腐烂Ⅳ级或Ⅴ级)腐殖化度最大。这对进一步认识高山森林生态系统植物-土壤互作过程具有重要意义。
高山森林粗木質殘體腐殖化是促進生態繫統土壤髮育和碳吸存的主要途徑之一,併可能受到腐爛等級和木質殘體類型的影響,但一直缺乏必要的關註。因此,在2013年8月,以青藏高原東緣海拔3600 m左右的高山森林中具有代錶性的岷江冷杉(Abies faxoniana)原始林為研究對象,根據區域內坡度和物種組成設置3箇100 m×100 m的典型樣地,在研究樣地內隨機選取5箇腐爛等級的岷江冷杉粗木質殘體,每箇腐爛等級3株,4種粗木質殘體,共計60株,調查和研究區域內不同腐爛等級倒木、枯立木、根樁和大枯枝等主要類型粗木質殘體的腐殖化特徵。結果錶明:枯立木、大枯枝和倒木腐殖質碳、鬍敏痠碳和富裏痠碳含量隨腐爛等級增加而增大,而根樁腐殖質碳、鬍敏痠碳和富裏痠碳含量隨腐爛等級增加而減小,併且枯立木在各箇分解階段腐殖質碳、鬍敏痠碳和富裏痠碳含量均保持較高水平。同時,枯立木、大枯枝和倒木的腐殖化度隨腐爛等級增加呈增大趨勢,根樁腐殖化度卻隨著腐爛等級增加而減小,其腐殖化度分彆為52.93%~85.88%、49.2%~73.68%、54.94%~67.21%和53.41%~68.68%。枯立木腐殖化度明顯高于其他3種類型粗木質殘體,且在腐殖化後期(腐爛Ⅳ級或Ⅴ級)腐殖化度最大。這對進一步認識高山森林生態繫統植物-土壤互作過程具有重要意義。
고산삼림조목질잔체부식화시촉진생태계통토양발육화탄흡존적주요도경지일,병가능수도부란등급화목질잔체류형적영향,단일직결핍필요적관주。인차,재2013년8월,이청장고원동연해발3600 m좌우적고산삼림중구유대표성적민강랭삼(Abies faxoniana)원시림위연구대상,근거구역내파도화물충조성설치3개100 m×100 m적전형양지,재연구양지내수궤선취5개부란등급적민강랭삼조목질잔체,매개부란등급3주,4충조목질잔체,공계60주,조사화연구구역내불동부란등급도목、고립목、근장화대고지등주요류형조목질잔체적부식화특정。결과표명:고립목、대고지화도목부식질탄、호민산탄화부리산탄함량수부란등급증가이증대,이근장부식질탄、호민산탄화부리산탄함량수부란등급증가이감소,병차고립목재각개분해계단부식질탄、호민산탄화부리산탄함량균보지교고수평。동시,고립목、대고지화도목적부식화도수부란등급증가정증대추세,근장부식화도각수착부란등급증가이감소,기부식화도분별위52.93%~85.88%、49.2%~73.68%、54.94%~67.21%화53.41%~68.68%。고립목부식화도명현고우기타3충류형조목질잔체,차재부식화후기(부란Ⅳ급혹Ⅴ급)부식화도최대。저대진일보인식고산삼림생태계통식물-토양호작과정구유중요의의。
Humification of coarse woody debris was one of the main pathways of soil formation and carbon sequestration in alpine forest ecosystems, where type of coarse woody debris and decay class could play an important role in coarse woody debris humification thanks to its insulation effect. However, the results were still not clear which limit the understanding and response of coarse woody debris humification. Therefore, three 100 m×100 m plots were sampled in a Minjiang fir (Abies faxoniana) primary forest ecosystem around 3600 m altitude in western Sichuan in August, 2013. In order to explore effects of type of coarse woody debris and different decay class, we investigated different decay class fallen logs, snags, stumps and large branches, each decay class of coarse woody debris and collected altogether 60 trees. Results clearly showed that: snag, fallen log and large branch of humus carbon, humic acid and fulvic acid carbon content increased with the change of decay levels, whereas snag humus carbon, humic acid and fulvic acid carbon content was maintaining decline. At the same time, snag, stump, large branch, fallen log, which humification degree respectively 52.93%~85.88%, 49.2%~73.68%, 54.94%~67.21% and 53.41%~68.68%. Snag, its humification degree was significantly higher than the other three types of coarse woody debris, and humification degree was the highest in the late humification (IV decay class or V decay class). For further understanding about the alpine forest ecosystem of plant and soil interaction process which is of great significance.