Temporal dynamics and vertical distribution of dissolved organic carbon in snowmelt runoff in a temperate deciduous forest in Maoershan region, northeastern China.

ZHANG Zhu; WANG Chuan-kuan.

doi:10.13332/j.1000-1522.20160114

Journal of Beijing Forestry University > 2016 > 38(11): 1-8. > DOI: 10.13332/j.1000-1522.20160114

ZHANG Zhu, WANG Chuan-kuan.. Temporal dynamics and vertical distribution of dissolved organic carbon in snowmelt runoff in a temperate deciduous forest in Maoershan region, northeastern China.[J]. Journal of Beijing Forestry University, 2016, 38(11): 1-8. DOI: 10.13332/j.1000-1522.20160114

Citation:

PDF (1112 KB)

Temporal dynamics and vertical distribution of dissolved organic carbon in snowmelt runoff in a temperate deciduous forest in Maoershan region, northeastern China.

Center for Ecological Research, Northeast Forestry University, Harbin, Heilongjiang, 150040, P. R. China.

More Information

Received Date: April 07, 2016
Published Date: November 29, 2016

Graphical Abstract

Abstract

Abstract

The dissolved organic carbon (DOC) during snowmelt period is crucial to analyzing carbon outputs from terrestrial ecosystems to rivers by streamflow in northern regions. The aim of this work was to quantify temporal dynamics and vertical distribution of DOC concentration and flux in snowmelt runoffs. A water balance plot with an area of 625 m2 was established in a typical temperate deciduous forest in Maoershan Forest Ecosystem Research Station, northeastern China, and the snowmelt runoffs and DOC concentrations at four different soil depths (5, 35, 65, and 95 cm) were measured in 2014. The results showed that: 1) the inputs of water and DOC into the soil during the snowmelt period were 74.2 mm and 0.25 g/m2, respectively, while the outputs were 15.6 mm and 0.22 g/m2, respectively. The runoff rate reached approximately 21%, but the input and output of DOC were roughly balanced. 2) The relationships between DOC concentration and instantaneous water flow rate varied with soil depths during the peak period of snowmelt. DOC concentration and instantaneous water flow rate were not correlated significantly (P0.05) at 5 and 35 cm soil depths, but significantly, negatively correlated at 65 cm soil depth (R2=0.29, P0.05) and positively at 95 cm soil depth (R2=0.43, P0.05). The instantaneous DOC flux and water flow rate were significantly, linearly correlated for all the soil depths (R20.9,P0.001), and the greater the instantaneous water flow rates were, the steeper the slopes of the linear equations for the soil layers were, suggesting a hydrologically driven DOC loss. 3) Both DOC and water exported at different soil depths during the snowmelt period followed the order of 35 cm5 cm65 cm95 cm. The amount of water and DOC exported at 5 and 35 cm soil depths accounted for 70% of the total in the soil profile. The variability in DOC concentrations tended to converge to low concentration with the soil depth increasing due to the effect of soil retention.
- carbon loss,
- snowmelt runoff,
- temporal dynamics,
- vertical distribution,
- temperate forest

FullText(HTML)

References (37)

References

[1]	GREN A, HAEI M, KOHLER S, et al. Regulation of stream water dissolved organic carbon (DOC) concentrations during snowmelt: the role of discharge, winter climate and memory effects[J]. Biogeosciences,2010, 7(9): 2901-2913.
[1]
[2]	COLE J J, PRAIRIE Y T, CARACO N F, et al. Plumbing the global carbon cycle: integrating inland waters into the terrestrial carbon budget[J]. Ecosystems, 2007, 10(1): 172-185.
[2]	LIU H L, CAI T J, MAN X L, et al.Effects of major forest types of Xiaoxing'an Mountains on the process of snowfall, snow cover and snow melting[J]. Journal of Beijing Forestry University, 2012, 34(2): 20-25.
[3]	ZHANG Q Z, WANG C K. Carbon density and distribution of six Chinese temperate forests[J]. Sci China Life Sci, 2010, 40(7): 621-631.
[3]	DEMERS J D, DRISCOLL C T, SHANLEY J B. Mercury mobilization and episodic stream acidification during snowmelt: role of hydrologic flow paths, source areas, and supply of dissolved organic carbon[J]. Water Resources Research,2010, 46(1): W01511.
[4]	XIONG L, YANG Y S, ZHU J M, et al.Transport characteristics of dissolved organic carbon in different soil horizons in natural Castanopsis carlesii forest[J]. Acta Ecologica Sinica,2015, 35(17): 5711-5720.
[4]	SANDFORD R C, HAWKINS J M, BOL R, et al. Export of dissolved organic carbon and nitrate from grassland in winter using high temporal resolution, in situ UV sensing[J]. Science of the Total Environment,2013, 456-457: 384-391.
[5]	刘海亮,蔡体久,满秀玲,等. 小兴安岭主要森林类型对降雪、积雪和融雪的影响[J]. 北京林业大学学报, 2012, 34(2): 20-25.
[5]	LIU S, YU G R, JUN A S, et al. The thawing-freeing processes and soil moisture distribution of the steppe in central Mongolian Plateau[J]. Acta Pedologica Snica, 2009, 46(1): 46-51.
[6]	PROKUSHKIN A S, POKROVSKY O S, SHIROKOVA L S, et al. Sources and the flux pattern of dissolved carbon in rivers of the Yenisey Basin draining the Central Siberian Plateau[J]. Environmental Research Letters,2011, 6: 045212.
[7]	WINTERDAHL M, ERLANDSSON M, FUTTER M N, et al. Intra-annual variability of organic carbon concentrations in running waters: drivers along a climatic gradient [J]. Global Biogeochemical Cycles, 2014, 28(4): 451-464.
[8]	KIM S B, SHIN H J, PARK M, et al. Assessment of future climate change impacts on snowmelt and stream water quality for a mountainous high-elevation watershed using SWAT[J]. Paddy and Water Environment, 2015, 13(4): 557-569.
[9]	YUCEL I, GUVENTURK A, SEN O L. Climate change impacts on snowmelt runoff for mountainous transboundary basins in eastern Turkey[J]. International Journal of Climatology,2015, 35(2): 215-228.
[10]	PEICHL M, MOORE T R, ARAIN M A, et al. Concentrations and fluxes of dissolved organic carbon in an age-sequence of white pine forests in Southern Ontario, Canada[J]. Biogeochemistry, 2007, 86(1): 1-17.
[11]	HUA K K, ZHU B, WANG X G. Dissolved organic carbon loss fluxes through runoff and sediment on sloping upland of purple soil in the Sichuan Basin[J]. Nutrient Cycling in Agroecosystems, 2014, 98(2): 125-135.
[12]	GROFFMAN P M, DRISCOLL C T, FAHEY T J, et al. Effects of mild winter freezing on soil nitrogen and carbon dynamics in a northern hardwood forest[J]. Biogeochemistry, 2001, 56(2): 191-213.
[13]	LEMMA B, NILSSON I, KLEJA D B, et al. Decomposition and substrate quality of leaf litters and fine roots from three exotic plantations and a native forest in the southwestern highlands of Ethiopia[J]. Soil Biology and Biochemistry,2007, 39(9): 2317-2328.
[14]	LESSELS J S, TETZLAFF D, CAREY S K, et al. A coupled hydrology-biogeochemistry model to simulate dissolved organic carbon exports from a permafrost-influenced catchment[J]. Hydrological Processes, 2015: 29(26): 1085-1099.
[15]	KOCH J, RUNKEL R, STRIEGL R, et al. Hydrologic controls on the transport and cycling of carbon and nitrogen in a boreal catchment underlain by continuous permafrost[J]. Journal of Geophysical Research: Biogeosciences, 2013, 118(2): 698-712.
[16]	SEBESTYEN S D, BOYER E W, SHANLEY J B, et al. Sources, transformations, and hydrological processes that control stream nitrate and dissolved organic matter concentrations during snowmelt in an upland forest[J]. Water Resources Research,2008, 44: W12410.
[17]	TIPPING E, WOOF C, RIGG E, et al. Climatic influences on the leaching of dissolved organic matter from upland UK moorland soils, investigated by a field manipulation experiment[J]. Environment International, 1999, 25(1): 83-95.
[18]	LIU W, XU X, MCGOFF N M, et al. Spatial and seasonal variation of dissolved organic carbon (DOC) concentrations in Irish streams: importance of soil and topography characteristics[J]. Environmental Management,2014, 53(5): 959-967.
[19]	HOLMES R M, MCLELLAND J W, PETERSON B J, et al. Seasonal and annual fluxes of nutrients and organic matter from large rivers to the Arctic Ocean and surrounding seas[J]. Estuaries and Coasts, 2012, 35(2): 369-382.
[20]	WANG C, HAN Y, CHEN J Q, et al. Seasonality of soil CO2 efflux in a temperate forest: biophysical effects of snowpack and spring freeze-thaw cycles[J]. Agricultural and Forest Meteorology, 2013, 177: 83-92.
[21]	张全智, 王传宽. 6种温带森林碳密度与碳分配[J]. 中国科学:生命科学, 2010, 40(7): 621-631.
[22]	STROHMEIER S, KNORR K H, REICHERT M, et al. Concentrations and fluxes of dissolved organic carbon in runoff from a forested catchment: insights from high frequency measurements[J]. Biogeosciences, 2013, 10(2): 905-916.
[23]	FUJII K, UEMURA M, HAYAKAWA C, et al. Fluxes of dissolved organic carbon in two tropical forest ecosystems of East Kalimantan, Indonesia[J]. Geoderma, 2009, 152(1): 127-136.
[24]	PELLERIN B A, SARACENO J F, SHANLEY J B, et al. Taking the pulse of snowmelt: in situ sensors reveal seasonal, event and diurnal patterns of nitrate and dissolved organic matter variability in an upland forest stream[J]. Biogeochemistry,2012, 108(1-3): 183-198.
[25]	熊丽, 杨玉盛, 朱锦懋, 等. 可溶性有机碳在米槠天然林不同土层中的迁移特征[J]. 生态学报,2015,35(17):5711-5720.
[26]	刘帅, 于贵瑞, 浅沼顺, 等. 蒙古高原中部草地土壤冻融过程及土壤含水量分布[J]. 土壤学报, 2009, 46(1): 46-51.
[27]	USELMAN S M, QUALLS R G, LILIENFEIN J. Contribution of root vs. leaf litter to dissolved organic carbon leaching through soil[J]. Soil Science Society of America Journal, 2007, 71(5): 1555-1563.
[28]	MICHALZIK B, MATZNER E. Dynamics of dissolved organic nitrogen and carbon in a Central European Norway spruce ecosystem[J]. European Journal of Soil Science,1999, 50(4): 579-590.
[29]	MCCLAIN M E, BOYER E W, DENT C L, et al. Biogeochemical hot spots and hot moments at the interface of terrestrial and aquatic ecosystems[J]. Ecosystems, 2003, 6(4): 301-312.
[30]	ROBSON T M, LAVOREL S, CLEMENT J C, et al. Neglect of mowing and manuring leads to slower nitrogen cycling in subalpine grasslands[J]. Soil Biology and Biochemistry,2007, 39(4): 930-941.
[31]	LAUDON H, SJBLOM V, BUFFAM I, et al. The role of catchment scale and landscape characteristics for runoff generation of boreal streams[J]. Journal of Hydrology, 2007, 344(3): 198-209.
[32]	SHANLEY J B, KENDALL C, SMITH T E, et al. Controls on old and new water contributions to stream flow at some nested catchments in Vermont, USA[J]. Hydrological Processes,2002,16(3):589-609.

Cited By

Cited by

Periodical cited type(9)

1.	赵一鸣，徐文，安容容，王淼，李沁泽，张颖超. 饲料中单宁、硫代葡萄糖苷和植酸对畜禽的影响及其降解方法. 饲料工业. 2024(07): 119-125 .
2.	李淼，胡文泽，岳国鑫，郭东旭，石莹，荣海峰，郑徽，马凤鸣. 高聚原花青素降解技术研究进展. 食品工业科技. 2022(07): 417-423 .
3.	高洁，赵妍. 黑苦荞麦壳高聚原花青素降解及其抗氧化活性分析. 食品研究与开发. 2022(12): 147-154 .
4.	吕筱，郑天元，韦新月，窦子珊，高晨佳，蔡冉，孟琬星，王汝华. 花生红衣中原花青素的提取工艺与活性研究. 农产品加工. 2021(09): 27-31 .
5.	姜坤，叶焕烽，叶秦轩，杨海花. 响应面法优化多聚原飞燕草素超声波降解工艺及其抗氧化性的研究. 食品工业科技. 2021(13): 221-229 .
6.	高晨曦，黄艳，孙威江. 茶叶中原花青素研究进展. 茶叶科学. 2020(04): 441-453 .
7.	国田，张娜，符群，柴洋洋，郭庆启. 几种辅助提取方式对蓝莓原花青素浸提效果及抗氧化活性的影响. 北京林业大学学报. 2020(09): 139-148 . 本站查看
8.	李特，宋见喜，张卓睿，姜贵全. 缩合单宁降解方法研究进展. 林产化学与工业. 2020(05): 10-16 .
9.	卜得新，张方艳，朱桂兰，郭娜，鲁红侠. 几种深色食物中原花青素含量及抗氧化活性的测定和比较. 农产品加工. 2019(15): 66-69 .

Other cited types(5)

Get Citation

PDF

XML

Article views (1628) PDF downloads (26) Cited by(14)

Turn off MathJax

Article Contents

Abstract

References

Temporal dynamics and vertical distribution of dissolved organic carbon in snowmelt runoff in a temperate deciduous forest in Maoershan region, northeastern China.

Abstract

References

Cited by

Periodical cited type(9)

Other cited types(5)

Catalog

Export File

Citation

Format

Content