生态环境学报 ›› 2022, Vol. 31 ›› Issue (12): 2283-2291.DOI: 10.16258/j.cnki.1674-5906.2022.12.002
收稿日期:
2022-09-06
出版日期:
2022-12-18
发布日期:
2023-02-15
通讯作者:
*作者简介:
宋瑞朋(1996年生),男,硕士研究生,主要研究方向为森林土壤有机碳组分。E-mail: songruipeng8@163.com
基金资助:
SONG Ruipeng1(), YANG Qifan1, ZHENG Zhiheng1, XI Dan1,2,*
Received:
2022-09-06
Online:
2022-12-18
Published:
2023-02-15
摘要:
林下植被作为影响森林土壤有机碳储量的重要因子之一,探讨其类型对土壤有机碳组分的影响,以期为人工林林下植被管理及可持续经营提供理论依据。以杉木(Cunninghamia lanceolata)人工林3种林下优势植被——箬竹(Indocalamus tessellatus)、双盖蕨(Diplazium donianum)和紫麻(Oreocnide frutescens)为对象,测定不同土层(0—10、10—20、20—40、40—60、60—80 cm)土壤总有机碳、惰性有机碳、易氧化有机碳、微生物生物量碳和可溶性有机碳的质量分数特征,分析各有机碳组分在林下植被、土层间的差异性。结果表明,(1)3种林下植被土壤总有机碳、惰性有机碳和微生物生物量碳的质量分数沿剖面均呈显著下降趋势,易氧化有机碳在0—10 cm土层均值最高,可溶性有机碳表现出先增后降的分布特征。(2)总有机碳在40—60 cm土层表现为箬竹(8.94 g?kg?1)显著高于双盖蕨(7.00 g?kg?1);0—10、10—20 cm土层惰性有机碳质量分数最高的分别是紫麻(18.66 g?kg?1)和双盖蕨(11.38 g?kg?1);箬竹表层土壤微生物生物量碳占比最高(2.35%)。(3)相关性分析表明,土壤有机碳组分均与全氮、C/N值、可溶性总氮以及微生物生物量氮呈极显著正相关(P<0.01);各有机碳组分两两之间均呈极显著正相关关系(P<0.01)。(4)RDA分析表明,10—20、20—40 cm土层对各有机碳组分影响最显著的环境因子是微生物生物量氮(E=47.9%、53.1%),而在40—60 cm土层中影响最显著的是全氮(E=43.6%)。林下植被类型主要显著影响表层土壤有机碳组分,惰性有机碳在林下植被类型间的差异更显著。紫麻和双盖蕨能促进表层土壤稳定性碳的积累,而箬竹覆盖下的表层土壤有机碳组分具有较快的分解转化速率。
中图分类号:
宋瑞朋, 杨起帆, 郑智恒, 习丹. 3种林下植被类型对杉木人工林土壤有机碳及其组分特征的影响[J]. 生态环境学报, 2022, 31(12): 2283-2291.
SONG Ruipeng, YANG Qifan, ZHENG Zhiheng, XI Dan. Effects of Three Understory Vegetation Types on Soil Organic Carbon and Its Components in Cunninghamia lanceolata Plantation[J]. Ecology and Environment, 2022, 31(12): 2283-2291.
林下植被Understory vegetation | 高度 Height/ cm | 地径 Ground diameter/ cm | 坡向 Slope aspect | 坡位 Slope position | 温度 Temperature/℃ | 海拔Altitude/m | 多度Abundance/% | 其他林下植被 Other undergrowth vegetation |
---|---|---|---|---|---|---|---|---|
It | 44.2±1.4 | 0.53±0.1 | 西南 | 下坡 | 18.96 | 110±3 | 90.3±0.7% | 闽楠(Phoebe bournei)、淡竹叶(Lophatherum gracile)和双盖蕨等 |
Dd | 108.3±13.0 | 5.80±1.1 | 西南 | 中坡 | 19.05 | 125±3 | 83.1±2.5% | 枇杷叶紫珠(Callicarpa kochiana)、闽楠、箬竹、紫麻、铁芒萁(Dicranopteris linearis)等 |
Of | 130.8±4.6 | 1.7±0.68 | 西南 | 上坡 | 18.91 | 130±3 | 79.0±5.7% | 闽楠、箬竹、双盖蕨、网脉酸藤子(Embelia rudis Hand.-Mazz)、枇杷叶紫珠、铁芒萁、地菍(Melastoma dodecandrum)等 |
表1 样地信息表
Table 1 Information sheet of sample site
林下植被Understory vegetation | 高度 Height/ cm | 地径 Ground diameter/ cm | 坡向 Slope aspect | 坡位 Slope position | 温度 Temperature/℃ | 海拔Altitude/m | 多度Abundance/% | 其他林下植被 Other undergrowth vegetation |
---|---|---|---|---|---|---|---|---|
It | 44.2±1.4 | 0.53±0.1 | 西南 | 下坡 | 18.96 | 110±3 | 90.3±0.7% | 闽楠(Phoebe bournei)、淡竹叶(Lophatherum gracile)和双盖蕨等 |
Dd | 108.3±13.0 | 5.80±1.1 | 西南 | 中坡 | 19.05 | 125±3 | 83.1±2.5% | 枇杷叶紫珠(Callicarpa kochiana)、闽楠、箬竹、紫麻、铁芒萁(Dicranopteris linearis)等 |
Of | 130.8±4.6 | 1.7±0.68 | 西南 | 上坡 | 18.91 | 130±3 | 79.0±5.7% | 闽楠、箬竹、双盖蕨、网脉酸藤子(Embelia rudis Hand.-Mazz)、枇杷叶紫珠、铁芒萁、地菍(Melastoma dodecandrum)等 |
图2 不同林下植被土壤总有机碳质量分数和有机碳密度 不同大写字母表示土层间差异显著,不同小写字母表示林下植被类型间差异显著(P<0.05),下同
Figure 2 Soil total organic carbon content and density of soil organic carbon in different understory vegetation Different capital letters indicate significant differences between soil layers, and different lowercase letters indicate significant differences between understory vegetation types at 0.05 level. The same below
图4 不同林下植被土壤惰性有机碳质量分数及其占总有机碳比例
Figure 4 Mass fraction and proportion of soil inert organic carbon in total organic carbon of different understory vegetation
图5 不同林下植被类型土壤有机碳及其组分与理化因子的冗余分析
Figure 5 Redundancy analysis of soil organic carbon and its components with physicochemical factors in different forest understory vegetation types
Index | pH | SWC | TN | C/N | NO3−-N | DTN | MBN | TOC | ROC | ROOC | DOC | MBC | Index |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
TOC | 0.491** | 0.372** | 0.985** | 0.877** | 0.506** | 0.766** | 0.905** | TOC | |||||
ROC | 0.548** | 0.390** | 0.931** | 0.854** | 0.502** | 0.699** | 0.911** | 0.959** | ROC | ||||
ROOC | 0.464** | 0.363** | 0.695** | 0.657** | 0.440** | 0.640** | 0.757** | 0.737** | 0.766** | ROOC | |||
DOC | 0.079 | 0.111 | 0.599** | 0.597** | 0.137 | 0.760** | 0.582** | 0.594** | 0.464** | 0.348** | DOC | ||
MBC | 0.459** | 0.202 | 0.874** | 0.772** | 0.379** | 0.645** | 0.946** | 0.878** | 0.863** | 0.672** | 0.562** | MBC | |
AOC | 0.471** | 0.359** | 0.729** | 0.686** | 0.444** | 0.665** | 0.792** | 0.768** | 0.791** | 0.998** | 0.388** | 0.714** | AOC |
表2 土壤有机碳组分与理化因子的相关系数
Table 2 Correlation coefficientsbetween soil carbon components with soil physical and chemical factors
Index | pH | SWC | TN | C/N | NO3−-N | DTN | MBN | TOC | ROC | ROOC | DOC | MBC | Index |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
TOC | 0.491** | 0.372** | 0.985** | 0.877** | 0.506** | 0.766** | 0.905** | TOC | |||||
ROC | 0.548** | 0.390** | 0.931** | 0.854** | 0.502** | 0.699** | 0.911** | 0.959** | ROC | ||||
ROOC | 0.464** | 0.363** | 0.695** | 0.657** | 0.440** | 0.640** | 0.757** | 0.737** | 0.766** | ROOC | |||
DOC | 0.079 | 0.111 | 0.599** | 0.597** | 0.137 | 0.760** | 0.582** | 0.594** | 0.464** | 0.348** | DOC | ||
MBC | 0.459** | 0.202 | 0.874** | 0.772** | 0.379** | 0.645** | 0.946** | 0.878** | 0.863** | 0.672** | 0.562** | MBC | |
AOC | 0.471** | 0.359** | 0.729** | 0.686** | 0.444** | 0.665** | 0.792** | 0.768** | 0.791** | 0.998** | 0.388** | 0.714** | AOC |
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