生态环境学报
生態環境學報
생태배경학보
ECOLOGY AND ENVIRONMENT
2014年
12期
1924-1932
,共9页
李琛琛%刘宁%郭晋平%张芸香%杨三红%白晋华
李琛琛%劉寧%郭晉平%張蕓香%楊三紅%白晉華
리침침%류저%곽진평%장예향%양삼홍%백진화
氮沉降%华北落叶松%树叶特性%土壤理化特性%模拟试验%短期影响
氮沉降%華北落葉鬆%樹葉特性%土壤理化特性%模擬試驗%短期影響
담침강%화북락협송%수협특성%토양이화특성%모의시험%단기영향
nitrogen deposition%Larix principis-rupprechtii%soil nutrient%leaf traits%simulation experiment%short term effect
以50 a生华北落叶松天然次生林为研究对象,采用全生长季野外多水平林地施氮对比试验的方法,结合树叶特性和林下土壤理化性质测定,设置对照(CK,0 g·m-2·a-1)、低氮(LN,8 g·m-2·a-1)、高氮(HN,15 g·m-2·a-1)3个施氮水平,进行短期氮沉降模拟试验,分析了短期氮沉降对华北落叶松针叶及林下0~10、10~20 cm两层土壤中土壤营养动态的影响,为华北落叶松林的群落结构优化调整、可持续经营管理提供理论依据。研究结果表明:为期一个生长季的短期施氮显著增加了华北落叶松林下0~20 cm土壤层中TOC、NH4+-N、NO3–-N的含量,却未影响土壤pH值和TN含量,且对表层(0~10 cm)土壤的影响更明显,但整个生长季内月份间的变化较大。短期施氮也导致50 a生华北落叶松针叶的宽度(W)、长度(L)、氮含量(LN)、比叶面积(SLA)和投影面积(PA)显著增加,但未影响叶生物量(LM)和叶有机碳含量(LC)。同时,叶氮含量与0~20 cm层、10~20 cm层土壤中全氮含量以及10~20 cm层土壤中NH4+-N含量显著正相关,叶有机碳含量则与0~20 cm层土壤有机碳含量和0~10 cm层土壤全氮含量亦呈正相关关系。以上结果说明,华北落叶松天然次生林处于氮限制状态,短期氮沉降可能会提高土壤肥力并促进树木的生长,有利于华北落叶松天然次生林生产力的提高。
以50 a生華北落葉鬆天然次生林為研究對象,採用全生長季野外多水平林地施氮對比試驗的方法,結閤樹葉特性和林下土壤理化性質測定,設置對照(CK,0 g·m-2·a-1)、低氮(LN,8 g·m-2·a-1)、高氮(HN,15 g·m-2·a-1)3箇施氮水平,進行短期氮沉降模擬試驗,分析瞭短期氮沉降對華北落葉鬆針葉及林下0~10、10~20 cm兩層土壤中土壤營養動態的影響,為華北落葉鬆林的群落結構優化調整、可持續經營管理提供理論依據。研究結果錶明:為期一箇生長季的短期施氮顯著增加瞭華北落葉鬆林下0~20 cm土壤層中TOC、NH4+-N、NO3–-N的含量,卻未影響土壤pH值和TN含量,且對錶層(0~10 cm)土壤的影響更明顯,但整箇生長季內月份間的變化較大。短期施氮也導緻50 a生華北落葉鬆針葉的寬度(W)、長度(L)、氮含量(LN)、比葉麵積(SLA)和投影麵積(PA)顯著增加,但未影響葉生物量(LM)和葉有機碳含量(LC)。同時,葉氮含量與0~20 cm層、10~20 cm層土壤中全氮含量以及10~20 cm層土壤中NH4+-N含量顯著正相關,葉有機碳含量則與0~20 cm層土壤有機碳含量和0~10 cm層土壤全氮含量亦呈正相關關繫。以上結果說明,華北落葉鬆天然次生林處于氮限製狀態,短期氮沉降可能會提高土壤肥力併促進樹木的生長,有利于華北落葉鬆天然次生林生產力的提高。
이50 a생화북락협송천연차생림위연구대상,채용전생장계야외다수평임지시담대비시험적방법,결합수협특성화림하토양이화성질측정,설치대조(CK,0 g·m-2·a-1)、저담(LN,8 g·m-2·a-1)、고담(HN,15 g·m-2·a-1)3개시담수평,진행단기담침강모의시험,분석료단기담침강대화북락협송침협급림하0~10、10~20 cm량층토양중토양영양동태적영향,위화북락협송림적군락결구우화조정、가지속경영관리제공이론의거。연구결과표명:위기일개생장계적단기시담현저증가료화북락협송림하0~20 cm토양층중TOC、NH4+-N、NO3–-N적함량,각미영향토양pH치화TN함량,차대표층(0~10 cm)토양적영향경명현,단정개생장계내월빈간적변화교대。단기시담야도치50 a생화북락협송침협적관도(W)、장도(L)、담함량(LN)、비협면적(SLA)화투영면적(PA)현저증가,단미영향협생물량(LM)화협유궤탄함량(LC)。동시,협담함량여0~20 cm층、10~20 cm층토양중전담함량이급10~20 cm층토양중NH4+-N함량현저정상관,협유궤탄함량칙여0~20 cm층토양유궤탄함량화0~10 cm층토양전담함량역정정상관관계。이상결과설명,화북락협송천연차생림처우담한제상태,단기담침강가능회제고토양비력병촉진수목적생장,유리우화북락협송천연차생림생산력적제고。
In a natural secondary forest ofLarix principis-rupprechtii (~50 years old), 3 nitrogen addition levels (0 g·m-2·a-1, 8 g·m-2·a-1, 15 g·m-2·a-1) were setup and applied in one growing season to simulate the short term nitrogen deposition. Our objectives were to determine the effects of increased nitrogen deposition on soil nutrient dynamics in such stand and the needle responses of Larix principis-rupprechtii and their relationships by continuous monitoring of soil physicochemical properties and measuring leaf traits of current year needles. The results showed: the short-term nitrogen addition significantly increased NH4+-N, NO3–-N, and Total Organic Carbon (TOC) contents in the 0~20 cm horizon and more pronounced in the 0~10 cm horizon, but not the soil pH and soil total nitrogen content (TN), while significant monthly variations were present. Nitrogen addition also increased the needle width (W), length (L), nitrogen content (LN), specific leaf area (SLA) and projected area (PA), but had no effects on needle biomass (LM) and needle carbon content (LC). Furthermore, LN was positively correlated with TN in the 0~20 cm and 10~20 cm horizons as well as NH4+-N in the 10~20 cm horizon respectively, while LC was positively related to TOC in the 10~20 cm horizon and TN in the 0~10 cm horizon respectively. In conclusion, the results suggested that the natural secondaryLarixprincipis-rupprechtiiforest is currently N-limited, even the short-term nitrogen input may improve the soil fertility and be beneficial to the absorption and utilization of trees, thus may potentially promote the productivity of such forest.