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茂兰喀斯特原生林不同坡向及分解层的凋落物现存量和养分特征

赵畅1,龙健1*,李娟2,廖洪凯1,刘灵飞1,张明江1,华健1   

  1. 1贵州师范大学贵州省山地环境重点实验室, 贵阳 550001; 2贵州师范大学地理与环境科学学院, 贵阳 550001)
  • 出版日期:2018-02-10 发布日期:2018-02-10

Litter stock and nutrient characteristics of decomposing litter layers in Maolan Karstprimary forest in different slope directions.

ZHAO Chang1, LONG Jian1*, LI Juan2, LIAO Hong-kai1, LIU Ling-fei1, ZHANG Ming-jiang1, HUA jian1   

  1. (1Guizhou Key Laboratory ofMountain Environment, Guizhou Normal University, Guiyang 550001, China; 2Department ofGeography and Environmental Science, Guizhou Normal University, Guiyang 550001, China).
  • Online:2018-02-10 Published:2018-02-10

摘要: 以茂兰喀斯特原生林3种坡向林下凋落物为研究对象,通过野外调研采样和室内分析测试相结合的方法,探讨了不同喀斯特原生林生态系统下坡向和分解层的凋落物现存量、主要营养元素含量、储量及元素释放率的分布特征。结果表明:1)阴坡凋落物现存总量((0.568±0.024) kg·m-2)高于阳坡((0.504±0.03) kg·m-2)和半阴坡((0.295±0.02)kg·m-2),不同坡向林下凋落物现存量在各分解层均表现为:未分解层(L层)>半分解层(F层)>全分解层(Y层);2)不同坡向林下凋落物各营养元素平均含量表现为:C((388.7±11.2)g·kg-1)>N((24.90±3.49) g·kg-1)>K((9.78±1.82) g·kg-1)>P((1.53±0.32)g·kg-1),在各分解层的含量表现不同,碳含量和钾含量:L>F>Y,氮含量和磷含量:Y>F>L;3)3种坡向林下凋落物的碳、氮、钾元素总储量表现为:阴坡>阳坡>半阴坡,磷元素总储量表现为:阳坡>阴坡>半阴坡;4)凋落物营养元素储量在L层占总储量的37.1%~64.2%,并随分解加剧而减少;L层和F层的元素释放率均表现为:阴坡>半阴坡>阳坡,且碳、钾元素释放率高于氮、磷元素。在喀斯特原生林凋落物分解的养分释放过程中,坡向对林下凋落物的理化性质及分解速率有较大影响,且阴坡林下凋落物分解较快、营养元素内部循环周期较短。

关键词: 燃烧试验, 土壤温度场, 采伐迹地, 长白落叶松人工林

Abstract: In the present study, we selected forest floor litters from three slope directions inMaolan Karst primary forest to investigate the distribution characteristics of litter stock, nutrientcontents (C, N, P and K) and their release rates of different decomposing layers. The results showed that: (1) Total litter stock was higher in north slope (0.568 kg·m-2) than that in south slope (0.504 kg·m-2) and northeast slope (0.295 kg·m-2). Litter stocks in different layers arranged in the order of fresh litter layer (layer L>fragmented litter layer (layer F) > fullydecomposed layer (layer Y); (2) The C and K contents in different decomposing layers were in the order of layer L>layer F>layer Y, whereas the N and P contents were followed by the order of layer Y> layer F> layer L. (3) Total storage of litter C, N and K was in the order of north slope>south slope>northeast slope, and total litter P storage was the highest in the south slope, followed by north slope, and then the northeast slope. (4) The litter nutrient storage in layer Laccounted for 37.1% to 64.2% of the total nutrient storage, showing a decrease trend with theincreases of decomposition degrees. The release rates of the nutrient elements in layers L and F were the highest in the north slope, followed by the northeast slope and the south slope.Moreover, the release rates of C and K were higher than that of N and P. Our results indicated that the slope direction had a great influence on the chemical properties and decomposition rate oflitters. In general, litters in the north slope decomposed rapidly and the cycling time of nutrient elements was shorter than that in other slopes in the Karst primary forest.

Key words: harvested site, Larix olgensis plantation, combustion experiment, soil temperature field