林业科学
林業科學
임업과학
SCIENTIA SILVAE SINICAE
2014年
6期
1-9
,共9页
郭宝华%刘广路%范少辉%杜满义%苏文会
郭寶華%劉廣路%範少輝%杜滿義%囌文會
곽보화%류엄로%범소휘%두만의%소문회
毛竹林%碳%氮%磷%分配格局%计量参数
毛竹林%碳%氮%燐%分配格跼%計量參數
모죽림%탄%담%린%분배격국%계량삼수
Phyllostachys edulis forest%C%N%P%distribution pattern%stoichiometric parameter
以南亚热带中心分布区的毛竹林为研究对象,比较不同生产力水平(Ⅰ:30000±1000 kg·hm -2 a -1;Ⅱ:34000±1000 kg·hm -2 a -1;Ⅲ:37000±1000 kg·hm -2 a -1;Ⅳ:42000±1000 kg·hm -2 a -1;Ⅴ:47000±1000 kg·hm -2 a -1)毛竹林植被和土壤的碳、氮、磷含量及计量特征,探讨生产力水平对毛竹林及土壤碳、氮、磷分布格局及化学计量特征的影响。结果表明:生产力水平对毛竹林植被碳和磷元素在不同器官间分配比例的影响较小,对氮素分配比例的影响较大;除竹叶碳元素分配比例在不同生产力水平间的差异达到显著水平外(P <0.01),各器官间碳、磷含量在不同生产力水平间差异均不显著;除竹秆外,毛竹不同器官氮分配比例在不同生产力水平间的差异均极显著(P<0.01);生产力水平对毛竹林植被 C∶N、C∶P、N∶P计量比值的影响较小,在不同生产力水平间的差异均未达到显著水平(P<0.01),毛竹林主要养分元素的计量比具有内在的稳定性,符合“内稳性假说”;生产力水平对林地土壤碳、氮、磷、水解氮和有效磷含量有显著影响,土壤 C∶N、C∶P、N∶P 和 H-N∶A-P 在不同生产力间的差异均达到了极显著水平(P<0.01);当土壤N∶P<14时,主要受到氮元素的限制,本研究中土壤N∶P为4.50~13.89,反映了研究区毛竹林主要受到氮元素的限制,受磷元素的限制较少,且 N∶P 比值随着生产力的提高呈降低的趋势,有可能成为未来毛竹林退化诊断的生态指示指标;毛竹林植被主要养分计量值与土壤主要养分计量值的相关性分析表明,二者间的相关性未达到显著水平。
以南亞熱帶中心分佈區的毛竹林為研究對象,比較不同生產力水平(Ⅰ:30000±1000 kg·hm -2 a -1;Ⅱ:34000±1000 kg·hm -2 a -1;Ⅲ:37000±1000 kg·hm -2 a -1;Ⅳ:42000±1000 kg·hm -2 a -1;Ⅴ:47000±1000 kg·hm -2 a -1)毛竹林植被和土壤的碳、氮、燐含量及計量特徵,探討生產力水平對毛竹林及土壤碳、氮、燐分佈格跼及化學計量特徵的影響。結果錶明:生產力水平對毛竹林植被碳和燐元素在不同器官間分配比例的影響較小,對氮素分配比例的影響較大;除竹葉碳元素分配比例在不同生產力水平間的差異達到顯著水平外(P <0.01),各器官間碳、燐含量在不同生產力水平間差異均不顯著;除竹稈外,毛竹不同器官氮分配比例在不同生產力水平間的差異均極顯著(P<0.01);生產力水平對毛竹林植被 C∶N、C∶P、N∶P計量比值的影響較小,在不同生產力水平間的差異均未達到顯著水平(P<0.01),毛竹林主要養分元素的計量比具有內在的穩定性,符閤“內穩性假說”;生產力水平對林地土壤碳、氮、燐、水解氮和有效燐含量有顯著影響,土壤 C∶N、C∶P、N∶P 和 H-N∶A-P 在不同生產力間的差異均達到瞭極顯著水平(P<0.01);噹土壤N∶P<14時,主要受到氮元素的限製,本研究中土壤N∶P為4.50~13.89,反映瞭研究區毛竹林主要受到氮元素的限製,受燐元素的限製較少,且 N∶P 比值隨著生產力的提高呈降低的趨勢,有可能成為未來毛竹林退化診斷的生態指示指標;毛竹林植被主要養分計量值與土壤主要養分計量值的相關性分析錶明,二者間的相關性未達到顯著水平。
이남아열대중심분포구적모죽림위연구대상,비교불동생산력수평(Ⅰ:30000±1000 kg·hm -2 a -1;Ⅱ:34000±1000 kg·hm -2 a -1;Ⅲ:37000±1000 kg·hm -2 a -1;Ⅳ:42000±1000 kg·hm -2 a -1;Ⅴ:47000±1000 kg·hm -2 a -1)모죽림식피화토양적탄、담、린함량급계량특정,탐토생산력수평대모죽림급토양탄、담、린분포격국급화학계량특정적영향。결과표명:생산력수평대모죽림식피탄화린원소재불동기관간분배비례적영향교소,대담소분배비례적영향교대;제죽협탄원소분배비례재불동생산력수평간적차이체도현저수평외(P <0.01),각기관간탄、린함량재불동생산력수평간차이균불현저;제죽간외,모죽불동기관담분배비례재불동생산력수평간적차이균겁현저(P<0.01);생산력수평대모죽림식피 C∶N、C∶P、N∶P계량비치적영향교소,재불동생산력수평간적차이균미체도현저수평(P<0.01),모죽림주요양분원소적계량비구유내재적은정성,부합“내은성가설”;생산력수평대임지토양탄、담、린、수해담화유효린함량유현저영향,토양 C∶N、C∶P、N∶P 화 H-N∶A-P 재불동생산력간적차이균체도료겁현저수평(P<0.01);당토양N∶P<14시,주요수도담원소적한제,본연구중토양N∶P위4.50~13.89,반영료연구구모죽림주요수도담원소적한제,수린원소적한제교소,차 N∶P 비치수착생산력적제고정강저적추세,유가능성위미래모죽림퇴화진단적생태지시지표;모죽림식피주요양분계량치여토양주요양분계량치적상관성분석표명,이자간적상관성미체도현저수평。
Phyllostachys edulis forests and soil in their central distribution area in subtropical China were selected as research object. This study discussed the effects of productivity level (Ⅰ: 30 000 ± 1 000 kg·hm -2 a -1;Ⅱ: 34 000 ± 1 000 kg·hm -2 a -1;Ⅲ:37 000 ± 1 000 kg·hm -2 a -1;Ⅳ:42 000 ± 1 000 kg·hm -2 a -1;Ⅴ:47 000 ± 1 000 kg·hm -2 a -1 ) on the distribution of carbon ( C ) , nitrogen ( N ) and phosphorus ( P ) and their stoichiometric characteristics of Phyllostachys edulis and soil by comparing C,N and P content of Phyllostachys edulis and soil,and their stoichiometric characteristics,which could provide theory evidence for long-term productivity maintenance in Phyllostachys edulis forests. The result showed that the productivity level had less effect on the distribution of plant C and P in different organs,and had more effects on N distribution. The difference of the distribution pattern of C and P of each organ in different productivity levels was not significant,except leaf C (P<0. 01). Except bamboo stem,N distribution pattern in different organs in different productivity levels reached a highly significant level ( P <0. 01 ) . The productivity levels had less impact on the stoichiometry of plant C∶N,C∶P and N∶P,the difference in different productivity levels did not reach a significant level. Stoichiometry of main nutrients in Phyllostachys edulis forests was inherently stable, in line with “internal stability hypothesis”. The productivity levels had significant impact on soil C,N,P,hydrolyzable N and available P,soil C∶ N,C∶ P,N∶ P,H-N∶ A-P reached a highly significant level in different productivity levels ( P <0. 01). When N∶P < 14,the forests was mainly limited by N. In this study,soil N∶P was 4. 50 -13. 89,indicating Phyllostachys edulis forests in research area was mainly limited by N,rather than P. N∶P decreased with the increase of productivity level,soil N∶P was index to represent Phyllostachys edulis forests degradation succession process. Analysis the correlation between stoichiometry value of main nutrient of plant and soil indicated no significant level between the two.