1. 西南林业大学生态与环境学院,昆明,650224
2. 国家林业和草原局云南玉溪森林生态系统国家定位观测研究站,昆明,650224
[ "肖文贤(1991-),女,在读硕士研究生,主要从事森林生态系统水文功能研究。E-mail:845388187@qq.com" ]
纸质出版:2023
移动端阅览
肖文贤, 王克勤, 宋娅丽, 等. 氮沉降下滇中高原森林凋落物分解特征对其持水性的影响[J]. 水土保持学报, 2023,37(1):227-237.
XIAO Wenxian, WANG Keqin, SONG Yali, et al. Influence of Decomposition Characteristics of Forest Litter on Water Holding Capacity Under Nitrogen Deposition in Central Yunnan Plateau[J]. 2023, 37(1): 227-237.
肖文贤, 王克勤, 宋娅丽, 等. 氮沉降下滇中高原森林凋落物分解特征对其持水性的影响[J]. 水土保持学报, 2023,37(1):227-237. DOI: 10.13870/j.cnki.stbcxb.2023.01.030.
XIAO Wenxian, WANG Keqin, SONG Yali, et al. Influence of Decomposition Characteristics of Forest Litter on Water Holding Capacity Under Nitrogen Deposition in Central Yunnan Plateau[J]. 2023, 37(1): 227-237. DOI: 10.13870/j.cnki.stbcxb.2023.01.030.
研究模拟氮沉降下凋落物分解特征对其持水性的影响
旨在为氮沉降背景下森林生态系统养分循环和水分循环相关研究提供理论依据。以滇中高原常绿阔叶林和高山栎林为研究对象
在野外开展模拟氮沉降下凋落叶、枝原位分解研究试验
设置0(对照CK)
10(低氮LN)
20(中氮MN)
25(高氮HN) g/(m2·a)N共4种处理
利用尼龙网袋法和室内浸泡法
探究不同处理下凋落叶、枝质量残留率、持水量和持水率及吸水速率变化特征。结果表明:(1) 2种林分凋落叶、枝质量残留率随分解时间延长而减少;与CK质量残留率相比
LN处理2种林分凋落叶、枝无显著影响(p>0.05)
MN和HN处理使常绿阔叶林凋落叶分解第16
19
23
24个月和HN处理高山栎林凋落叶分解第16个月分别增加5.05%~7.45%
7.88%~8.62%
4.72%。(2)与CK分解95%所需时间相比
LN处理使常绿阔叶林凋落叶、枝和高山栎林凋落枝分别增加0.549
0.366
0.402年
高山栎林凋落叶则减少1.011年
MN和HN处理使2种林分落叶、枝增加0.236~3.638年。(3)分解时间和氮沉降及其二者交互作用显著影响凋落叶、枝最大持水量、最大持水率和最大吸水速率(p<0.001);与CK最大持水量、最大持水率和最大吸水速率相比
LN和MN处理使常绿阔叶林凋落叶分别减少21.99%
6.47%
54.47%
16.14%
4.15%
1.25%
HN处理分别增加0.24%
0.80%
0.96%
LN、MN和HN处理使常绿阔叶林凋落枝和高山栎林凋落叶、枝分别增加8.03%~38.22%
5.47%~60.00%
0.46%~5.72%。(4) 2种林分凋落叶、枝持水量和持水率与浸泡时间呈对数函数关系(m=a+bln t)
吸水速率与浸泡时间呈幂函数关系(v=at-b)。(5)常绿阔叶林凋落叶和高山栎林凋落枝质量残留率分别与其最大持水量、最大持水率和最大吸水速率呈显著正相关关系(p<0.05)。综上
凋落物持水性受其分解阶段和氮沉降干扰的影响。
To study the influence of decomposition characteristics of litter on their water holding capacity under simulated nitrogen (N) deposition so as to provide a theoretical basis for the study of nutrient and water cycling in forest ecosystem under N deposition. The evergreen broad-leaved forest and Quercus semicarpifolia forest in central Yunnan Plateau were selected to conduct in situ leaf litter and twig decomposition experiment with four N treatment levels of 0 (control check CK)
10 (low nitrogen LN)
20 (medium nitrogen MN) and 25 (high nitrogen HN) g/(m2·a)N. Litterbag method and the laboratory immersion method were used to explore the variation characteristics of mass remaining rate
water holding capacity
water holding rate and water absorption rate of leaf litter and twig litter under different treatment. The results showed that: (1) The mass remaining rate of leaf litter and twig litter in two forest types decreased with the extension of decomposition time. Compared with the mass remaining rate of CK
LN treatment had no significant effect on leaf litter and twig litter in two forest types. MN and HN treatments increased leaf litter decomposition in evergreen broad-leaved forest at 16
19
23
24 months and HN treatment increased leaf litter decomposition in Q. semicarpifolia forest at 16 months by 5.05%~7.45%
7.88%~8.62% and 4.72%
respectively. (2) Compared with the CK
LN treatment increased the time required for 95% decomposition of leaf litter and twig litter in evergreen broad-leaved forest and twig litter in Q. semicarpifolia forest by 0.549
0.366 and 0.402 years
respectively
while that of leaf litter in Q. semicarpifolia forest decreased by 1.011 years
and that of leaf litter and twig litter in two forest types under MN and HN treatment increased by 0.236~3.638 years. (3) The decomposition time
nitrogen deposition and their interaction significantly affected the maximum water holding capacity
maximum water holding rate
maximum water absorption of leaf litter and twig litter (p<0.001). Compared with the CK
the maximum water holding capacity
maximum water holding rate
maximum water absorption of leaf litter in evergreen broad-leaved forest under LN and MN treatments decreased by 21.99%
6.47%
54.47%
16.14%
4.15% and 1.25%
respectively
and those under HN treatment increased by 0.24%
0.80%
and 0.96%
respectively
and in LN and MN and HN treatments
those of twig litter in evergreen broad-leave forest and leaf and twig litter in Q. semicarpifolia forest increased by 8.03%~38.22%
5.47%~60.00% and 0.46%~5.72%
respectively. (4) The relationship between water holding capacity and the water holding rate of leaf litter and twig litter in two forest types and immersion time was a logarithmic function (m=a+bln t)
and the water absorption rate was exponentially related to immersion time (v=at-b). (5) The mass remaining rate of leaf litter in evergreen broad-leaved forest and that of twig litter in Q. semicarpifolia forest were significantly and positively correlated with their maximum water holding capacity
maximum water holding rate and maximum water absorption rate
respectively (p<0.05). In conclusion
the water holding capacity of litter was affected by the decomposition stage and nitrogen deposition.
Zhao Y H, Zhang L, Chen Y F, et al. Atmospheric nitrogen deposition to China:A model analysis on nitrogen budget and critical load exceedance[J].Atmospheric Environment,2017,153:32-40.
冯憬,张相锋,董世魁,等.增温与氮沉降对高寒植物净光合速率的影响[J].草业科学,2018,35(4):781-790.
许庆民,周赓,郭小伟,等.青藏高原高寒草甸群落特征对氮沉降和增水的响应[J].草原与草坪,2017,37(5):8-13.
Jing H, Wang G L. Temporal dynamics of
Pinus tabulaeformis
litter decomposition under nitrogen addition on the Loess Plateau of China[J].Forest Ecology and Management,2020,476:e118465.
张晓曦,胡嘉伟,王丽洁,等.不同林龄刺槐林地凋落物分解及养分释放对氮沉降的响应差异[J].植物资源与环境学报,2021,30(6):10-18.
文海燕,傅华,郭丁.黄土高原典型草原优势植物凋落物分解及养分释放对氮添加的响应[J].生态学报,2017,37(6):2014-2022.
Hou S L, Hättenschwiler S, Yang J J, et al. Increasing rates of long-term nitrogen deposition consistently increased litter decomposition in a semi-arid grassland[J].New Phytologist,2021,229(1):296-307.
Chen F S, Wang G G, Fang X M, et al. Nitrogen deposition effect on forest litter decomposition is interactively regulated by endogenous litter quality and exogenous resource supply[J].Plant and Soil,2019,437(1):413-426.
张建利,吴华,喻理飞,等.草海湿地流域优势树种凋落物叶分解与水文特征研究[J].水土保持学报,2014,28(3):98-103.
王忠禹,刘国彬,王兵,等.黄土丘陵区典型植物枯落物凋落动态及其持水性[J].生态学报,2019,39(7):2416-2425.
周祥,赵一鹤,张洪江,等.云南高原典型林分林下枯落物持水特征研究[J].生态环境学报,2011,20(2):248-252.
吴迪,韩振诚,李苇洁,等.马缨杜鹃不同花叶比例凋落物的分解程度和持水性能研究[J].水土保持学报,2020,34(5):186-191.
蒲嘉霖,刘亮.亚热带森林凋落物分解特征及水文效应[J].水土保持研究,2019,26(6):165-170.
王东丽,郝可欣,梁潇洒,等.干扰对固沙樟子松林凋落物特征及持水性的影响[J].浙江农林大学学报,2019,36(6):1125-1133.
周世兴,黄从德,向元彬,等.模拟氮沉降对华西雨屏区天然常绿阔叶林凋落物木质素和纤维素降解的影响[J].应用生态学报,2016,27(5):1368-1374.
刘济明,唐子燕,李佳,等.氮沉降对米槁凋落叶分解过程中土壤养分的影响[J].甘肃农业大学学报,2021,56(1):102-108,117.
潘禹.滇中亚高山典型森林凋落物分解及土壤微生物量碳氮对模拟氮沉降的响应[D].昆明:西南林业大学,2021.
Wang Q, Kwak J H, Choi W J, et al. Long-term N and S addition and changed litter chemistry do not affect trembling aspen leaf litter decomposition, elemental composition and enzyme activity in a boreal forest[J].Environmental Pollution,2019,250:143-154.
Song X Z, Zhou G M, Gu H H, et al. Management practices amplify the effects of N deposition on leaf litter decomposition of the Moso bamboo forest[J].Plant and Soil,2015,395(1):391-400.
张雨鉴,王克勤,宋娅丽,等.滇中亚高山地带性植被凋落物分解对模拟氮沉降的响应[J].生态学报,2020,40(22):8274-8286.
郭剑芬,杨玉盛,陈光水,等.森林凋落物分解研究进展[J].林业科学,2006,42(4):93-100.
刘文耀,刘伦辉,荆桂芬,等.云南松林与常绿阔叶林中枯落叶分解研究[J].云南植物研究,2000,22(3):298-306,316.
沈芳芳,刘文飞,吴建平,等.杉木人工林凋落物分解对氮沉降的响应[J].生态学报,2019,39(21):8078-8090.
铁烈华,符饶,张仕斌,等.模拟氮、硫沉降对华西雨屏区常绿阔叶林凋落叶分解速率的影响[J].应用生态学报,2018,29(7):2243-2250.
Pereira L C, Balbinot L, Lima M T, et al. Aspects of forest restoration and hydrology:The hydrological function of litter[J].Journal of Forestry Research,2022,33(2):543-552.
杜雪,王海燕,耿琦,等.云冷杉针阔混交林枯落物持水性能[J].水土保持学报,2021,35(2):361-368.
Santos A F A, Carneiro A C P, Martinez D T, et al. Capacidade de retenção hídrica do estoque de serapilheira de eucalipto[J].Floresta e Ambiente,2017,24:e89723022.
0
浏览量
749
下载量
3
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621