1. 内蒙古农业大学沙漠治理学院,呼和浩特,010018
2. 内蒙古杭锦荒漠生态系统国家定位观测研究站,内蒙古,鄂尔多斯,017400
3. 中盐内蒙古化工股份有限公司盐碱分公司资源保护站,内蒙古,阿拉善,750336
[ "魏亚娟(1994-),女,博士研究生,主要从事荒漠化防治研究。E-mail:weiyajuan0305@163.com" ]
网络首发:2022-05-27,
纸质出版:2022
移动端阅览
魏亚娟, 汪季, 党晓宏, 等. 干旱荒漠区人工梭梭林土壤碳氮磷密度与生态化学计量特征[J]. 水土保持学报, 2022,36(3):259-266.
WEI Yajuan, WANG Ji, DANG Xiaohong, et al. Soil Carbon, Nitrogen and Phosphorus Densities and Ecological Stoichiometry Characteristics of[J]. 2022, 36(3): 259-266.
魏亚娟, 汪季, 党晓宏, 等. 干旱荒漠区人工梭梭林土壤碳氮磷密度与生态化学计量特征[J]. 水土保持学报, 2022,36(3):259-266. DOI: 10.13870/j.cnki.stbcxb.2022.03.037.
WEI Yajuan, WANG Ji, DANG Xiaohong, et al. Soil Carbon, Nitrogen and Phosphorus Densities and Ecological Stoichiometry Characteristics of[J]. 2022, 36(3): 259-266. DOI: 10.13870/j.cnki.stbcxb.2022.03.037.
为了阐明人工梭梭林土壤碳氮磷密度及其生态化学计量特征演变规律
以吉兰泰荒漠区不同林龄(3
6
11
16年)人工梭梭林为研究对象
分析0—20
20—40
40—60 cm土层土壤有机碳(SOC)、全氮(TN)、全磷(TP)密度和生态化学计量特征。结果表明:(1)4种林龄人工梭梭林0—60 cm土层SOC、TN含量及其密度随林龄增加而升高
而TP含量及其密度随林龄增加而降低。其中
3
6年梭梭林SOC、TN含量及其密度随土层深度增加而升高
TP含量及其密度则与之相反;11
16年梭梭林SOC、TN、TP含量及其密度随土层深度增加而降低。(2)4种林龄梭梭林土壤C∶N、C∶P、N∶P分别为2.24~9.21
1.59~7.05
0.56~0.81
均属于中等变异水平
且变异系数随林龄和土层深度增加逐渐减小
说明土壤C∶N、C∶P、[JP]N∶P趋于平稳状态。(3)林龄、土层深度及其交互作用显著影响SOC含量、SOC密度、C∶N、C∶P
对TN含量、TP含量、TN密度、TP密度、N∶P无显著影响。(4)土壤孔隙度(STP)与SOC密度呈显著正相关关系(P<0.05)
说明土壤孔隙度增加有助于SOC密度增加
提高土壤肥力。在干旱荒漠区建植梭梭林有利于提高土壤肥力
改善干旱荒漠区土壤环境。
To investigate the evolution of planting years on soil carbon
nitrogen
phosphorus densities
and eco-chemical stoichiometry in Halaxylon ammodendron plantations
an age sequence of H. ammodendron stands (3
6
11 and 16 years) were selected in desert area of Jilantai
densities and stoichiometry characteristics of soil organic carbon (SOC)
total nitrogen (TN)
total phosphorus (TP) at soil depths of 0-20
20-40
40-60 cm were measured. The results showed that:(1) The contents and densities of SOC and TN in 0-60 cm soil increased with the increase of stand age
whereas the content and density of TP decreased with the increase of stand age. The SOC and TN contents and densities increased with the increase of soil depth in 3-year and 6-year plantations
and the content and density of TP were moving in exactly the opposite direction. The contents and densities of SOC
TN and TP increased with the increase of soil depth in 11-year and 16-year plantations. (2) The C:N
C:P and N:P ratios were 2.24~9.21
1.59~7.05 and 0.56~0.81 with moderate spatial variation
and the coefficient of variation decreased with the stand age and soil depth
indicating that soil C:N
C:P and N:P ratios tended to remain stable. (3) Stand age
soil depth
and their interaction had a significant effect on SOC content
SOC density
C:N and C:P ratios
but had no significant effect on the N:P ratio and the contents and densities of TN and TP. (4) Soil porosity (STP) had a significant positive correlation with SOC density (P<0.05)
indicating that the increase of soil porosity is helpful to increase SOC density and improve soil fertility. Plantation of H. ammodendron can improve soil fertility and soil environment in arid desert area.
Yu Z P, Wang M H, Huang Z Q, et al. Temporal changes in soil C-N-P stoichiometry over the past 60 years across subtropical China[J].Global Change Biology,2018,24(3):1308-1320.
Qiao Y, Wang J, Liu H M, et al. Depth-dependent soil C-N-P stoichiometry in a mature subtropical broadleaf forest[J].Geoderma,2020,370:1-12.
Achat D L, Bakker M R, Augusto L, et al. Phosphorus status of soils from contrasting forested ecosystems in southwestern Siberia:Effects of microbiological and physicochemical properties[J].Biogeosciences,2013,10(2):733-752.
forest on Daiyun Mountain[J].Forests,2019,10(12):1089-1100.
Zhang Y, Li C, Wang M L. Linkages of C:N:P stoichiometry between soil and leaf and their response to climatic factors along altitudinal gradients[J].Jounal of Soils and Sediments,2019,19(4):1820-1829.
张元明,王雪芹.准噶尔荒漠生物结皮研究[M].北京:科学出版社,2008.
Chen H, Zhao X R, Chen X J. Seasonal changes of soil microbial C, N, P and associated nutrient dynamics in a semiarid grassland of north China[J].Applied Soil Ecology,2018,128:89-97.
高永.吉兰泰盐湖环境演化及沙害成因[J].干旱区研究,1996,13(4):54-56,66.
郭彧,汪季,党晓宏,等.吉兰泰盐湖不同造林方式下梭梭枝系构型特征分析[J].西北林学院学报,2020,35(3):36-42.
韩永伟,王堃,张汝民,等.吉兰泰地区退化梭梭蒸腾生态生理学特性[J].草地学报,2002,10(1):40-44.
陈婧.吉兰泰人工梭梭林下土壤养分和机械组成的时空分布规律[D].呼和浩特:内蒙古农业大学,2019.
鲍士旦.土壤农化分析[M].北京:中国农业出版社,2000.
Jobbágy E E G, Jackson R B. The vertical distribution of soil organic carbon and its relation to climate and vegetation[J].Ecology Applications,2000,10(2):423-436.
张芸,李惠通,张辉,等.不同林龄杉木人工林土壤C:N:P化学计量特征及其与土壤理化性质的关系[J].生态学报,2019,39(7):2520-2531.
淑敏,姜涛,王东丽,等.科尔沁沙地不同林龄樟子松人工林土壤生态化学计量特征[J].干旱区研究,2018,35(4):789-795.
张珂,陈永乐,高艳红,等.阿拉善荒漠典型植物功能群氮、磷化学计量特征[J].中国沙漠,2014,34(5):1261-1267.
伍方骥,刘娜,胡培雷,等.典型喀斯特洼地植被恢复过程中土壤碳氮储量动态及其对极端内涝灾害的响应[J].中国生态农业学报(中英文),2020,28(3):429-437.
魏红,满秀玲.中国寒温带不同林龄白桦林碳储量及分配特征[J].植物生态学报,2019,43(10):843-852.
孙小东,宁志英,杨红玲,等.中国北方典型风沙区土壤碳氮磷化学计量特征[J].中国沙漠,2018,38(6):1209-1218.
董雪,辛智鸣,黄雅茹,等.乌兰布和沙漠典型灌木群落土壤化学计量特征[J].生态学报,2019,39(17):6247-6256.
刘玉林,朱广宇,邓蕾,等.黄土高原植被自然恢复和人工造林对土壤碳氮储量的影响[J].应用生态学报,2018,29(7):2163-2172.
Li Y Q, Chen Y P, Wang X Y, et al. Improvements in soil carbon and nitrogen capacities after shrub planting to stabilize sand dunes in China's Horqin Sandy Land[J].Sustainability,2017,9(4):1-17.
何高迅,王越,彭淑娴,等.滇中退化山地不冋植被恢复下土壤碳氮磷储量与生态化学计量特征[J].生态学报,2020,40(13):4425-4435.
Viscarra R R A, Bui E N. A new detailed map of total phosphorus stocks in Australian soil[J].Science of the Total Environment,2016,542:1040-1049.
张继辉,蔡道雄,卢立华,等.不同林龄柚木人工林土壤生态化学计量特征[J].生态学报,2020,40(16):5718-5728.
陶冶,刘耀斌,吴甘霖,等.准噶尔荒漠区域尺度浅层土壤化学计量特征及其空间分布格局[J].草业学报,2016,25(7):13-23.
李红林,贡璐,朱美玲,等.塔里木盆地北缘绿洲土壤化学计量特征[J].土壤学报,2015,52(6):1345-1355.
董雪,郝玉光,辛智鸣,等.科尔沁沙地4种典型灌木灌丛下土壤碳、氮、磷化学计量特征[J].西北植物学报,2019,39(1):164-172.
0
浏览量
730
下载量
9
CSCD
关联资源
相关文章
相关作者
相关机构
京公网安备11010802024621