1. 西北农林科技大学水土保持研究所, 黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西 杨陵,712100
2. 中国科学院水利部水土保持研究所, 陕西 杨陵,712100
[ "王亚娟(1995—),女,汉族,甘肃会宁人,硕士研究生,主要从事流域管理研究。E-mail:3259225914@qq.com" ]
纸质出版:2022
移动端阅览
王亚娟, 陈云明, 孙亚荣, 等. 黄土丘陵区油松人工林植物器官—凋落物—土壤化学计量特征的季节变化[J]. 水土保持学报, 2022,36(4):350-356.
WANG Yajuan, CHEN Yunming, SUN Yarong, et al. Seasonal Variation of Plant Organ-Litter-Soil Stoichiometry in[J]. 2022, 36(4): 350-356.
王亚娟, 陈云明, 孙亚荣, 等. 黄土丘陵区油松人工林植物器官—凋落物—土壤化学计量特征的季节变化[J]. 水土保持学报, 2022,36(4):350-356. DOI: 10.13870/j.cnki.stbcxb.2022.04.043.
WANG Yajuan, CHEN Yunming, SUN Yarong, et al. Seasonal Variation of Plant Organ-Litter-Soil Stoichiometry in[J]. 2022, 36(4): 350-356. DOI: 10.13870/j.cnki.stbcxb.2022.04.043.
为了解黄土丘陵区油松人工林植物器官—凋落物—土壤的化学计量特征随季节的变化规律,通过时空替代法、野外调查取样与室内试验的手段,以陕西省延安市安塞区纸坊沟流域中林龄油松(Pinus tabuliformis)人工林为对象,分析了4—10月油松不同器官—凋落物—土壤的碳(C)、氮(N)、磷(P)生态化学计量学特征。结果表明:(1)从4—10月,叶片C、P含量逐渐上升,在10月最高,叶片的N含量和N:P及枝的N、P含量均先减小后增大,且均在8月最低,而枝的C:N及C:P和细根的C:P、N:P均先增大后减小,且均在8月最高。土壤C、N含量、C:P、N:P先增大后减小,在8月最高。凋落物N含量、C:P和N:P均呈先降后升的趋势,在6月最低,P含量变化不显著;(2)除叶片4—6月、细根4—8月N:P>14外,其他各器官4—10月均N:P<14,该区域油松生长主要受N限制;(3)叶片与凋落物的C、N含量及C:N之间均呈显著正相关,C:N、C:P与N:P之间均呈显著正相关(p<0.05)。叶片N:P与土壤C:N呈极显著负相关(p<0.01),其他化学计量特征之间均无显著相关性。凋落物C含量与土壤P含量呈显著正相关(p<0.05)。研究结果使人工林生态化学计量学的研究更加系统性,为黄土丘陵区植被良好生长提供参考依据。
To understand the seasonal variation of plant organs-litter-soil stoichiometry in Pinus tabulaeformis plantation in Loess Hilly region
the field investigation and laboratory experiments were used by means of spatio-temporal substitution method in Zhifanggou Watershed
Ansai District
Yan'an City
Shaanxi Province
China. The ecological stoichiometry characteristics of carbon (C)
nitrogen (N) and phosphorus (P) in different organs-litter-soil of Pinus tabulaeformis from April to October were analyzed. The results showed that:(1) From April to October
the contents of C and P in leaves increased gradually
and reached the highest in October. The contents of N and N:P in leaves and branches decreased first and then increased
and reached the lowest in August. While the contents ofC:N and C:P in branches and C:P and N:P in fine roots increased first and then decreased
and reached the highest in August. Soil C and N contents
C:P and N:P increased first and then decreased
and reached the highest value in August. Litter N content
C:P and N:P all showed a trend of decreasing first and then increasing
and reached the lowest in June
while P content had no significant change. (2) Except for N:P>14 in leaves from April to June and fine roots from April to August
N:P<14 in other organs from April to October
the growth of Pinus tabulaeflorus in this region was mainly restricted by N. (3) There were significant positive correlations between C and N contents and C:N of leaf and litter
and there were significant positive correlations between C:N
C:P and N:P (p<0.05). There was a significant negative correlation between leaf N:P and soil C:N (p<0.01)
but no significant correlation between other stoichiometric characteristics. There was a significant positive correlation between litter C content and soil P content (p<0.05). The results make the study of ecological stoichiometry of plantation more systematic and provide reference for vegetation growth in loess hilly region.
Elser J J, Hamilton A. Stoichiometry and the new biology:The future is now[J].PLoS Biology, 2007, 5(7):e181.
Han W X, Fang J Y, Guo D L, et al. Leaf nitrogen and phosphorus stoichiometry across 753 terrestrial plant species in China[J].New Phytologist, 2005, 168(2):377-385.
Klausmeier C A, Litchman E, Daufresne T, et al. Optimal nitrogen-to-phosphorus stoichiometry of phytoplankton[J].Nature, 2004, 429(6988):171-174.
Mcgroddy M E, Daufresne T, Hedin L O. Scaling of C:N:P stoichiometry in forests worldwide:Implications of terrestrial Redfield-type ratios[J].Ecology, 2004, 85(9):2390-2401.
Sardans J, Peñuelas J. The role of plants in the effects of global change on nutrient availability and stoichiometry in the Plant-Soil System[J].Plant Physiology, 2012, 160(4):1741-1761.
Zhao Q Q, Bai J H, Liu Q, et al. Spatial and seasonal variations of soil carbon and nitrogen content and stock in a Tidal Salt Marsh with Tamarix chinensis, China[J].Wetlands, 2015, 36(S1):145-152.
Ågren G I. Stoichiometry and nutrition of plant growth in natural communities[J].Annual Review of Ecology, Evolution, and Systematics, 2008, 39(1):153-170.
赵亚芳, 徐福利, 王渭玲, 等.华北落叶松根茎叶碳氮磷含量及其化学计量学特征的季节变化[J].植物学报, 2014, 49(5):560-568.
封焕英, 杜满义, 辛学兵, 等.华北石质山地侧柏人工林C、N、P生态化学计量特征的季节变化[J].生态学报, 2019, 39(5):1572-1582.
Liu F D, Liu Y H, Wang G M, et al. Seasonal variations of C:N:P stoichiometry and their trade-offs in different organs of Suaeda salsa in Coastal Wetland of Yellow River Delta, China[J].PLoS One, 2015, 10(9):e138169.
霍晓英, 彭守璋, 任婧宇, 等.陕西省油松林生产力动态及对未来气候变化的响应[J].应用生态学报, 2018, 29(2):412-420.
董从国, 乔雨宁, 曹扬, 等.黄土高原不同植被带油松人工林生态化学计量特征及其影响因素[J].西北林学院学报, 2020, 35(3):1-8.
姜沛沛, 曹扬, 陈云明, 等.不同林龄油松(
Pinus tabulaeformis
)人工林植物、凋落物与土壤C、N、P化学计量特征[J].生态学报, 2016, 36(19):6188-6197.
杨霞, 陈丽华, 郑学良.不同林龄油松人工林土壤碳、氮和磷生态化学计量特征[J].中国水土保持科学, 2021, 19(2):108-116.
章广琦, 张萍, 陈云明, 等.黄土丘陵区刺槐与油松人工林生态系统生态化学计量特征[J].生态学报, 2018, 38(4):1328-1336.
鲍士旦.土壤农化分析[M].3版.北京:中国农业出版社, 2000.
李征, 韩琳, 刘玉虹, 等.滨海盐地碱蓬不同生长阶段叶片C、N、P化学计量特征[J].植物生态学报, 2012, 36(10):1054-1061.
牛得草, 李茜, 江世高, 等.阿拉善荒漠区6种主要灌木植物叶片C:N:P化学计量比的季节变化[J].植物生态学报, 2013, 37(4):317-325.
Herbert D A, Williams M, Rastetter E B. A model analysis of N and P limitation on carbon accumulation in Amazonian secondary forest after alternate land-use abandonment[J].Biogeochemistry, 2003, 65(1):121-150.
衣宁, 赵文倩, 刘倩, 等.油松新生叶与老叶光合功能的比较[J].林业科技, 2014, 39(6):10-14.
刘万德, 苏建荣, 李帅锋, 等.云南普洱季风常绿阔叶林演替系列植物和土壤C、N、P化学计量特征[J].生态学报, 2010, 30(23):6581-6590.
Wardle D A, Walker L R, Bardgett R D. Ecosystem properties and forest decline in contrasting long-term chrono sequences[J].Science, 2004, 305(5683):509-513.
刘兴诏, 周国逸, 张德强, 等.南亚热带森林不同演替阶段植物与土壤中N、P的化学计量特征[J].植物生态学报, 2010, 34(1):64-71.
张文彦, 樊江文, 钟华平, 等.中国典型草原优势植物功能群氮磷化学计量学特征研究[J].草地学报, 2010, 18(4):503-509.
杨阔, 黄建辉, 董丹, 等.青藏高原草地植物群落冠层叶片氮磷化学计量学分析[J].植物生态学报, 2010, 34(1):17-22.
吴旭, 牛耀彬, 陈云明, 董从国, 乔雨宁.黄土丘陵区沙棘混交林叶片、凋落物、土壤碳氮磷化学计量特征[J].水土保持学报, 2021, 35(4):369-376.
白小芳, 徐福利, 王渭玲, 等.华北落叶松人工林土壤碳氮磷生态化学计量特征[J].中国水土保持科学, 2015, 13(6):68-75.
Deng J, Wang S, Ren C, et al. Nitrogen and phosphorus resorption in relation to nutrition limitation along the chronosequence of Black Locust (
Robinia pseudoacacia
L.) plantation[J].Forests, 2019, 10(3):e261.
任书杰, 于贵瑞, 陶波, 等.中国东部南北样带654种植物叶片氮和磷的化学计量学特征研究[J].环境科学, 2007, 28(12):2665-2673.
汪宗飞, 郑粉莉.黄土高原子午岭地区人工油松林碳氮磷生态化学计量特征[J].生态学报, 2018, 38(19):6870-6880.
Tian H Q, Chen G S, Zhang C, et al. Pattern and variation of C:N:P ratios in China's soils:A synthesis of observational data[J].Biogeochemistry, 2010, 98(1/3):139-151.
朱潮, 武利玉, 张崇庆, 等.兰州市北山典型侧柏人工林分叶片与土壤生态化学计量特征[J].水土保持学报, 2021, 35(4):361-368.
王维奇, 徐玲琳, 曾从盛, 等.河口湿地植物活体-枯落物-土壤的碳氮磷生态化学计量特征[J].生态学报, 2011, 31(23):134-139.
Wang K, Wang G G, Song L N, et al. Linkages between nutrient resorption and ecological stoichiometry and homeostasis along a chronosequence of Mongolian pine plantations[J/OL].Frontiers in Plant Science, 2021:1605. https://doi.org/10.3389/fpls.2021.692683.
0
浏览量
600
下载量
4
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621