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Frontiers of Forestry in China

ISSN 1673-3517

ISSN 1673-3630(Online)

CN 11-5728/S

Front Fore Chin    2009, Vol. 4 Issue (2) : 171-177    https://doi.org/10.1007/s11461-009-0025-3
RESEARCH ARTICLE
Generation of runoff characteristics over three time periods for four typical forests in Jinyun Mountain, Chongqing City, southwest China
Xiaoyuan CHU1(), Yujie WANG1, Yiping XIA2, Yun WU2, Lin CHEN2
1. School of Soil and Water Conservation, Beijing Forestry University, Beijing 100083, China; 2. Management Bureau of Jinyun Mountain National Nature Reserve, Chongqing 400700, China
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Abstract

In order to provide a basis for water conservation in the restoration of vegetation for an urban water resource area, we studied the generation of runoff characteristics in four typical forests over three time periods in Jinyun Mountain, Chongqing City, based on the observation data of rainfall and runoff processes during the period 2002-2005. The results show that: 1) Rainfall was distributed evenly during the years 2002-2005. Annual rainfall variability was 4.46% and coefficient of variation was 0.0618. Average monthly rainfall tended towards a normal distribution N (113.8, 45972). 2) Both precipitation and runoff can be clearly divided into a dry and a wet season. The dry season was from October to March and the wet season from April to September. Most of annual runoff of the four forest stands occurred in the wet season. The surface runoff in the wet season accounted for more than 85% of the annual runoff, and more than 75% of underground runoff. 3) Both peak values of surface runoff and underground runoff occurred in June. The relation between monthly rainfall and surface/underground runoff was fitted by the model W=aP2+bP+c. The order of annual surface runoff was as follows: Phyllostachys pubescens forest > shrub forest > mixed Pinus massoniana-broadleaf forest > evergreen broad-leaved forest. The annual underground runoff was evergreen broad-leaved forest > mixed Pinus massoniana-broadleaf forest >Phyllostachys pubescens forest > shrub forest. 4) Under similar rainstorms events, the order of the surface runoff coefficient was: evergreen broad-leaved forest < mixed Pinus massoniana-broadleaf forest < shrub forest < Phyllostachys pubescens forest. The underground runoff coefficient was: evergreen broad-leaved forest > mixed Pinus massoniana-broadleaf forest >Phyllostachys pubescens forest > shrub forest. The relation between rainstorms and surface runoff was fitted by the linear relationship: Q=mp-n. Both mixed Pinus massoniana-broadleaf forest and evergreen broad-leaved forest have better flood regulation effects on an annual and monthly basis and per individual rainstorm. The function of Phyllostachys pubescens forest is the worst on all three bases.

Keywords Jinyun Mountain      time periods      runoff characteristics     
Corresponding Author(s): CHU Xiaoyuan,Email:chuxiaoyuan126@126.com   
Issue Date: 05 June 2009
 Cite this article:   
Xiaoyuan CHU,Yujie WANG,Yiping XIA, et al. Generation of runoff characteristics over three time periods for four typical forests in Jinyun Mountain, Chongqing City, southwest China[J]. Front Fore Chin, 2009, 4(2): 171-177.
 URL:  
https://academic.hep.com.cn/ffc/EN/10.1007/s11461-009-0025-3
https://academic.hep.com.cn/ffc/EN/Y2009/V4/I2/171
standselevation /mslope/oslope aspectcanopy density/%undergrowth plant cover/%grass cover/%soil layer thickness/cmsoil texturelitter thickness/cm
mixed Pinus massoniana-broad-leaved forests76025NW0.8403099sandy loam3.5
evergreen broad-leaved forests82530NW0.84020121sandy loam3.4
Phyllostachys pubescens forests80010NW0.7105090sandy loam1.5
shrub forests8608NW0.856050120sandy loam4.5
Tab.1  Standard basic information of typical stands
standstree speciesundergrowth plant speciesherbaceous species
mixed Pinus massoniana-broadleaf forestsGordonia acuminate, Pinus massoniana, Symplocos setchuensis, Adinandra bockianaEurya japonica, Adinandra bockiana, Symplocos setchuensis, Neolitsea aurata, Diospyros morrisianaPteridiaceae, Woodwardia japonica, Diplopterygium glauca, Lophatherum gracile
evergreen broad-leaved forestsGordonia acuminate, Neolitsea aurata, Adinandra bockianaCastanopsis carlesii, Rhamnus esquirolii, Symplocos setchuensis, Eurya japonicaPteridiaceae, Woodwardia japonica, Lophatherum gracile
Phyllostachys pubescens forestsPhyllostachys pubescensMells indica, Smilax china, Ficus viren, Sarcandra glabraPteridiaceae, Oplismenus compositus, Pilea pumil, Commelina communis
shrub forestsSymplocos caudate, Lindera kwangtunensis, Alniphyllum fortunei, Neolitsea aurataMachilus nanmu, Cunninghamia lanceolat, Eurya japonicaPteridiaceae, Hemercocallis fulva, Crassocephalumraben, Conyza canadensis
Tab.2  Species composition of typical stands
Jan.Feb.Mar.Apr.MayJun.Jul.Aug.Sep.Oct.Nov.Dec.sum
2002101.626.874.9177.8265.1315.2141.5132.382.161.657.350.81487.0
200317.412.028.385.8214.9347.0194.265.2115.190.490.635.91296.8
200416.554.4124.796.7113.5158.4116.7182.9250.470.2104.134.61323.1
200512.925.668.187.9134.8153.0199.2312.5114.8175.054.516.11354.4
average monthly rainfall/mm37.129.774.0112.1182.1243.4162.9173.2140.699.376.634.41365.3
proportion/%2.722.185.428.2113.3417.8311.9312.6910.307.275.612.52100
Tab.3  Monthly distribution of rainfall in Jinyun Mountain during 2002–2005
Fig.1  Graph of normal distribution and average monthly rainfall
Fig.2  Rainfall and runoff in dry and wet seasons. a: surface runoff; b: underground runoff.
Fig.3  Changes in runoff from different forest types. a: surface runoff; b: underground runoff.
runoff typesstandsabccorrelation coefficient
surface runoffmixed Pinus massoniana-broadleaf forests0.00020.0209-0.97570.924
broad-leaved forests0.00050.0291-1.12880.952
Phyllostachys pubescens forests0.0005-0.04971.56320.931
shrub forests0.0005-0.06081.78370.931
underground runoffmixed Pinus massoniana-broadleaf forests0.00100.0494-1.89560.950
broad-leaved forests0.0027-0.220712.50000.913
Phyllostachys pubescens forests0.00010.01510.29570.900
shrub forests0.0004-0.06091.99070.937
Tab.4  Relations of monthly rainfall and monthly runoff
standsrainsurface runoffunderground runoff
rainfall/mmprecipitation time/hKrunoff depth /mmrunoff coefficientinitial abst- raction duration/minrunoff duration/hrunoff depth /mmrunoff coefficientinitial abst- raction duration/minrunoff duration/h
mixed Pinus massoniana-broadleaf forests54.914.533.467.00.136617.8924.60.45124.367.59
broad-leaved forests54.914.533.463.40.0688.617.6730.90.56113.372.31
Phyllostachys pubescens forests54.914.533.4617.10.3160.417.443.50.06230.723.45
shrub forests54.914.533.468.20.1560.515.461.40.03372.219.77
Tab.5  Characteristics of mean runoffs after 25 rainstorms of typical stands in study area
runoff typesstandsmncorrelation coefficientnumber of sample
surface runoffmixed Pinus massoniana-broadleaf forests0.18783.77430.90525
evergreen broad-leaved forests0.15915.32620.80125
Phyllostachys pubescens forests0.546514.43500.88825
shrub forests0.25156.53210.88525
underground runoffmixed Pinus massoniana-broadleaf forests0.782114.13400.83225
evergreen broad-leaved forests0.855311.40100.86925
Phyllostachys pubescens forests0.07360.09950.76025
shrub forests0.05191.18190.73025
Tab.6  Relations between rainstorm and runoff
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[1] CHENG Chen, WANG Yujie, WANG Yunqi, PAN Yujuan. Soil fractal features of typical forest stands in Jinyun Mountain, Chongqing City, Southwest China[J]. Front. For. China, 2007, 2(4): 429-435.
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