降雨季节亚热带常绿阔叶林透冠雨对土壤可溶性有机质的迁移作用

王宏宇; 吴福忠; 张耀艺; 郑旭灵; 吴捷录; 张雪; 张欣影

doi:10.13870/j.cnki.stbcxb.2024.04.009

您当前的位置：

首页 >

文章列表页 >

降雨季节亚热带常绿阔叶林透冠雨对土壤可溶性有机质的迁移作用

更新时间：2025-03-12

- 降雨季节亚热带常绿阔叶林透冠雨对土壤可溶性有机质的迁移作用
- Effects of Throughfall on the Migration of Soil Dissolved Organic Matter in Subtropical Evergreen Broad-leaved Forest During Rainfall Season
- 水土保持学报 2024年38卷第4期页码：181-189
- 作者机构：
  
  1. 福建师范大学地理科学学院, 湿润亚热带生态-地理过程教育部重点实验室,福州,350117
  2. 福建三明森林生态系统国家野外科学观测研究站,福建,三明,365002
- 作者简介：
  
  [ "王宏宇(2000—),男,在读硕士研究生,主要从事森林土壤研究。E-mail:whyfjnu@163.com" ]
- 基金信息：
  
  国家自然科学基金项目(32171641,32101509,32271633)
- DOI：10.13870/j.cnki.stbcxb.2024.04.009
  中图分类号： S715.3
- 纸质出版：2024
- 稿件说明：
移动端阅览
王宏宇, 吴福忠, 张耀艺, 等. 降雨季节亚热带常绿阔叶林透冠雨对土壤可溶性有机质的迁移作用[J]. 水土保持学报, 2024,38(4):181-189.

WANG Hongyu, WU Fuzhong, ZHANG Yaoyi, et al. Effects of Throughfall on the Migration of Soil Dissolved Organic Matter in Subtropical Evergreen Broad-leaved Forest During Rainfall Season[J]. 2024, 38(4): 181-189.
王宏宇, 吴福忠, 张耀艺, 等. 降雨季节亚热带常绿阔叶林透冠雨对土壤可溶性有机质的迁移作用[J]. 水土保持学报, 2024,38(4):181-189. DOI： 10.13870/j.cnki.stbcxb.2024.04.009.

WANG Hongyu, WU Fuzhong, ZHANG Yaoyi, et al. Effects of Throughfall on the Migration of Soil Dissolved Organic Matter in Subtropical Evergreen Broad-leaved Forest During Rainfall Season[J]. 2024, 38(4): 181-189. DOI： 10.13870/j.cnki.stbcxb.2024.04.009.

摘要

[目的] 作为森林土壤中活性最高的组分

可溶性有机质(DOM)不仅可以直接被微生物利用

还是生态系统中C、N、P等元素迁移的主要载体

其迁移过程受到透冠雨驱动的水力作用和溶解过程的影响。[方法] 通过野外原位控制透冠雨输入试验

以亚热带常绿阔叶林的砂质红壤为对象

对照林窗降雨

分析降雨季节森林透冠雨对不同土层土壤可溶性有机碳(DOC)、可溶性有机氮(DON)和可溶性有机磷(DOP)动态变化的影响。[结果] (1)相对于林窗降雨

整个降雨季节以透冠雨为载体输入到土壤的DOM显著增加(p<0.01)

DOC、DON和DOP浓度分别增加37.00%

93.47%

85.12%

DOC、DON和DOP通量分别增加20.76%

49.93%

61.55%

但通过40 cm深土壤后

其输出通量差异并不显著

表明土壤对透冠雨中DOM具有较强的吸收能力。(2)相较于林窗降雨

透冠雨显著降低土壤表层输入C/N的29.19%

C/P的26.00%

而无明显改变N/P

而经过40 cm深土壤后

透冠雨显著降低土壤40 cm深度输入C/N的19.35%

C/P的13.35%和N/P的7.45%。表明透冠雨DOM增加主要是因为吸收冠层中的DON与DOP

而在土壤中DOM减少部分主要集中在DOC与DOP。(3)土壤DOC与DOP表现为截留减少

而DON表现为富集增加。相较于林窗降雨

透冠雨显著增加0—40 cm土壤对DOC截留量的39.93%和DOP截留量的72.42%

显著减少对DON释放量的32.37%。[结论] 研究结果充分证明亚热带常绿阔叶林透冠雨能促进DOM的输入

有利于土壤各层次对DOM的吸收

对于生态系统可持续经营和管理具有一定的科学意义。

Abstract

[Objective] As the most active component in forest soil

dissolved organic matter (DOM) can not only be directly utilized by microorganisms

but also be the main carrier for the migration of C

P and other elements in the ecosystem. The migration process is influenced by the hydraulic interactions and dissolving processes driven by throughfall. [Methods] Using soil column microcosm in situ culture to analyze the effects of forest throughfall on the dynamics of dissolved organic carbon (DOC)

dissolved organic nitrogen (DON)

and dissolved organic phosphorus (DOP) across varying layers of sandy red soil during the rainy season. The study focused on a subtropical evergreen broad-leaved forest with rainfall as a control. [Results] (1) During the rainfall season

the DOM input of throughfall into soil increased significantly compared with rainfall(p<0.01). The concentrations of DOC

DON and DOP increased by 37.00%

93.47%

and 85.12%

respectively

and the fluxes of DOC

DON and DOP also increased by 20.76%

49.93%

and 61.55%

respectively. However

there was no significant difference in output fluxes after passing through the 40 cm deep soil

indicating a strong capacity of the soil to absorb DOM from throughfall. (2) Compared to rainfall

throughfall reduced the C/N and C/P ratios of the soil surface by 29.19% and 26.00%

respectively

without significantly affecting N/P ratios. After passing through 40 cm of soil

throughfall reduced the input C/N

C/P and N/P ratios of the soil by 19.35%

13.35% and 7.45%

respectively. The increase in DOM in throughfall was mainly due to the absorption of DON and DOP in the canopy

while the decrease in soil DOM was mainly concentrated in DOC and DOP. (3) Soil DOC and DOP showed a reduction in interception

while DON showed an increase in enrichment. Throughfall increased the interception of DOC and DOP in the 0-40 cm soil by 39.93% and 72.42%

respectively

and significantly reduced the release of DON by 32.37%. [Conclusion] These results demonstrate that throughfall in a subtropical evergreen broad-leaved forest can promote the input of DOM and facilitate its uptake at different soil depths

with implications for the sustainable management of ecosystems.

关键词

Keywords

references

HU A, CHOI M, TANENTZAP A J, et al. Ecological networks of dissolved organic matter and microorganisms under global change[J].Nature Communications,2022,13:e3600.

LØNBORG C, CARREIRA C, ABRIL G, et al. A glolal database of dissolved organic matter(DOM) concentration measurements in coastal waters( Coast DOM vl)[J]. Earth System Science Data,2024,16(2):1107-1119.

江明华,程建中,李心清,等.生物炭对农田土壤CO

排放的影响研究进展[J].地球与环境,2021,49(6):726-736. JIANG M H, CHENG J Z, LI X Q, et al. The effect of biochar on the farmland soil CO

emission: A review[J].Earth and Environment,2021,49(6):726-736.

PARKER G G. Throughfall and stemflow in the forest nutrient cycle[J]. Advances in Ecological Research, 1983,13:57-133.

尚妍萌,张杰,孟会生,等.不同施肥处理下采煤矿区复垦土壤微生物功能多样性与共现性特征[J].生态学杂志,2023,42(2):386-394. SHANG Y M, ZHANG J, MENG H S, et al. Soil microbial functional diversity and co-occurrence under different fertilization treatments in a reclaimed coal mining area[J].Chinese Journal of Ecology,2023,42(2):386-394.

黄家辉,刘苑秋,许青,等.不同降雨强度下庐山日本柳杉林冠层透冠雨延滞效应[J].中国水土保持科学,2023,21(1):29-36. HUANG J H, LIU W Q, XU Q, et al. Time lag effects of throughfall on the canopy of

Cryptomeria japonica

in Lushan Mountain under different rainfall intensity[J].Science of Soil and Water Conservation,2023,21(1):29-36.

NIU G X, YIN G G, MO X H, et al. Do long-term high nitrogen inputs change the composition of soil dissolved organic matter in a primary tropical forest?[J].Environmental Research Letters,2022,17(9):e095015.

VAN STAN J, STUBBINS A. Tree-DOM: Dissolved organic matter in throughfall and stemflow[J].Limnology and Oceanography Letters,2018,3(3):199-214.

张楠,储安婷,杨红强.碳交易机制下林业碳汇产品类别比较与价值核算模型甄别[J].中国人口·资源与环境,2022,32(11):146-155. ZHANG N, CHU A T, YANG H Q. Forestry carbon sequestration products and their value accounting models under carbon trading mechanism[J].China Population,Resources and Environment,2022,32(11):146-155.

王淑春,程然然,杜盛.黄土丘陵区2种典型林分降雨分配特征及其主要影响因素[J].水土保持学报,2022,36(3):173-180. WANG S C, CHENG R R, DU S. Characteristics and main influencing factors of rainfall partitioning in two typical forests in the Loess Hilly Region[J].Journal of Soil and Water Conservation,2022,36(3):173-180.

郑旭灵,魏文涛,张潇月,等.亚热带山地森林源头溪流米槠凋落叶分解的水溶性碳氮磷动态[J].水土保持学报,2022,36(6):309-315. ZHENG X L, WEI W T, ZHANG X Y, et al. Dynamics of water-soluble carbon, nitrogen and phosphorus content during litter decomposition of

Castanopsis carlesii

in headwaters of subtropical mountain forest[J].Journal of Soil and Water Conservation,2022,36(6):309-315.

魏文涛,倪祥银,岳楷,等.中亚热带不同类型米槠林凋落枝溶解性有机质动态及光谱学特性[J].应用生态学报,2022,33(8):2121-2128. WEI W T, NI X Y, YUE K, et al. Dissolved organic matter dynamics and spectral characteristics of twig litter from different

Castanopsis carlesii

forests in the middle subtropical region, China[J].Chinese Journal of Applied Ecology, 2022,33(8):2121-2128.

HUANG W G, KUZYAKOV Y, NIU S L, et al. Drivers of microbially and plant-derived carbon in topsoil and subsoil[J].Global Change Biology,2023,29(22):6188-6200.

HAN B J, CHEN L Y, XIAO K, et al. Characteristics of dissolved organic matter (DOM) in Chinese farmland soils under different climate zone types: A molecular perspective[J].Journal of Environmental Management, 2024,350:e119695.

BRÖDLIN D, KAISER K, HAGEDORN F. Divergent patterns of carbon, nitrogen, and phosphorus mobilization in forest soils[J].Frontiers in Forests and Global Change,2019,2:e66.

张捷,刘洋,张健,等.马尾松人工林林冠层对氮、磷、硫的截留效应[J].水土保持学报,2014,28(4):37-43. ZHANG J, LIU Y, ZHANG J, et al. Effect of canopy interception on nitrogen, phosphorus and sulfur in

Pinus massoniana

plantations[J].Journal of Soil and Water Conservation,2014,28(4):37-43.

HUI D F, YANG X T, DENG Q, et al. Soil C∶N∶P stoichiometry in tropical forests on Hainan Island of China: Spatial and vertical variations[J].Catena,2021,201:e105228.

LIANG K, BI Y F, HE B H, et al. Changes in quantity and quality of dissolved organic carbon in purple soil: Roles of land use and soil depth[J].Land Degradation and Development,2023,34(2):327-337.

ROTH V N, LANGE M, SIMON C, et al. Persistence of dissolved organic matter explained by molecular changes during its passage through soil[J].Nature Geoscience, 2019,12:755-761.

LUO X Z, HOU E Q, CHEN J Q, et al. Dynamics of carbon, nitrogen, and phosphorus stocks and stoichiometry resulting from conversion of primary broadleaf forest to plantation and secondary forest in subtropical China[J].Catena,2020,193(16):e104606.

宣美林,廖姝,岳楷,等.亚热带不同林龄次生林与杉木林土壤氮淋溶损失特征[J].水土保持学报,2023,37(6):283-289,297. XUAN M L, LIAO S, YUE K, et al. Soil nitrogen leaching loss characteristics of subtropical secondary forests of different ages and

Cunninghamia lanceolata

plantations[J].Journal of Soil and Water Conservation, 2023,37(6):283-289,297.

MC DONOUGH L K, ANDERSEN M S, BEHNKE M I, et al. A new conceptual framework for the transformation of groundwater dissolved organic matter[J].Nature Communications,2022,13:e2153.

WANG M M, GUO X W, ZHANG S, et al. Global soil profiles indicate depth-dependent soil carbon losses under a warmer climate[J].Nature Communications,2022,13:e5514.

张雪,王冬梅,温文杰,等.青藏高原-黄土高原过渡带人工林土壤生态化学计量特征[J].中国水土保持科学,2020,18(6):81-89. ZHANG X, WANG D M, WEN W J, et al. Ecological stoichiometric characteristics of plantation soil in the Tibetan Plateau-Loess Plateau transition zone[J].Science of Soil and Water Conservation, 2020,18(6):81-89.

马利芳,熊黑钢,孙迪,等.不同干扰程度下土壤有机质空间最优插值法研究[J].生态学报,2019,39(19):7153-7160. MA L F, XIONG H G, SUN D, et al. Research on a spatial optimal interpolation method of soil organic matter under different degrees of disturbance[J].Acta Ecologica Sinica,2019,39(19):7153-7160.

吕茂奎,谢锦升,林廷武,等.降雨对米槠次生林和杉木人工林林冠可溶性有机碳迁移的影响[J].水土保持学报,2014,28(5):134-138. LÜ M K, XIE J S, LIN T W, et al. Effects of rainfall on dissolved organic carbon of canopy transport in a secondary forest of

Castanopsis carlesii

and

Cunninghamia lanceolata

plantation[J].Journal of Soil and Water Conservation, 2014,28(5):134-138.

STUBBINS A, GUILLEMETTE F, VAN STAN II J T. Throughfall and stemflow: The crowning headwaters of the aquatic carbon cycle[M]. Cham: Springer, 2020:121-132.

LIU H F, XU H W, WU Y, et al. Effects of natural vegetation restoration on dissolved organic matter (DOM) biodegradability and its temperature sensitivity[J]. Water Research,2021,191:e116792.

焦宏哲,李欢,陈惠,等.增温、施氮对中亚热带杉木林土壤可溶性有机质的影响[J].土壤学报,2020,57(5):1249-1258. JIAO H Z, LI H, CHEN H, et al. Effects of soil warming and nitrogen addition on soil dissolved organic matter of

Cunninghamia lanceolata

plantations in subtropical China[J].Acta Pedologica Sinica,2020,57(5):1249-1258.

杨智榕,林伟盛,蒲晓婷,等.土壤增温对杉木幼林不同深度土壤溶液DOM的影响[J].亚热带资源与环境学报,2015,10(1):91-94. YANG Z R, LIN W S, PU X T, et al. Effect of soil warming on DOM of soil solution at different depths of Chinese fir young forest[J].Journal of Subtropical Resources and Environment,2015,10(1):91-94.

VÉDÈRE C, LEBRUN M, HONVAULT N, et al. How does soil water status influence the fate of soil organic matter: A review of processes across scales[J].Earth Science Reviews,2022,234:e104214.

浏览量

25378

下载量

CSCD

文章被引用时，请邮件提醒。

提交

工具集

关联资源

亚热带森林碳储量与固碳量的构成及影响因素——以武宁县为例

林火干扰下亚热带森林土壤胞外酶化学计量特征

亚热带不同林龄次生林与杉木林土壤氮淋溶损失特征

人工柠条林地土壤水分补给和消耗动态变化规律

北京密云水库油松人工林对降水分配的影响