*
 

iForest - Biogeosciences and Forestry

*

Comparative water balance study of forest and fallow plots

N Móricz (1)   , C Mátyás (1), I Berki (1), E Rasztovits (1), Z Vekerdy (3), Z Gribovszki (2)

iForest - Biogeosciences and Forestry, Volume 5, Issue 4, Pages 188-196 (2012)
doi: https://doi.org/10.3832/ifor0624-005
Published: Aug 02, 2012 - Copyright © 2012 SISEF

Research Articles


Increasing pressure on groundwater due to land use change (e.g., afforestation) and future climate change will alter the recharge of groundwater aquifers, causing shifts in water table levels and hence influencing the available groundwater resources. The effect of land use change on groundwater resources has initiated a major scientific debate during the last decades between foresters and experts in water management in Hungary and in several other countries. The aim of this study was to compare water balances of two different vegetation covers, a groundwater dependent oak forest and a nearby fallow area in the Hungarian Lowland. Water balance components for an oak and a fallow plots, exposed to similar weather conditions and with similar soils, were estimated and compared by calibrating the Hydrus 1-D model using measured soil water content and groundwater levels. The difference in the groundwater consumption was analyzed in details during dry and wet growing seasons. Transpiration at the fallow plot was only about two-thirds of that in the oak forest, while groundwater consumption was three times higher in the forest than at the fallow plot throughout the two-year study. During the dry growing season, the proportion of groundwater use from the total transpiration reached up to 90% at the oak plot. According to the model, in the dry growing season in 2007 both vegetation covers relied significantly on groundwater resources, while in 2008 the consumption of groundwater was notably reduced due to the wet weather at both plots.

  Keywords


Water Balance, Oak, Fallow, Groundwater Consumption

Authors’ address

(1)
N Móricz
C Mátyás
I Berki
E Rasztovits
Institute of Environmental and Earth Sciences, University of West Hungary, Sopron (Hungary)
(2)
Z Gribovszki
Institute of Geomatics and Civil Engineering, University of West Hungary, Sopron (Hungary)
(3)
Z Vekerdy
Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede (Netherlands)

Corresponding author

 
N Móricz
calvus17@gmail.com

Citation

Móricz N, Mátyás C, Berki I, Rasztovits E, Vekerdy Z, Gribovszki Z (2012). Comparative water balance study of forest and fallow plots. iForest 5: 188-196. - doi: 10.3832/ifor0624-005

Academic Editor

Marco Borghetti

Paper history

Received: Nov 19, 2011
Accepted: Jun 30, 2012

First online: Aug 02, 2012
Publication Date: Aug 29, 2012
Publication Time: 1.10 months

Breakdown by View Type

(Waiting for server response...)

Article Usage

Total Article Views: 55395
(from publication date up to now)

Breakdown by View Type
HTML Page Views: 46961
Abstract Page Views: 3082
PDF Downloads: 3958
Citation/Reference Downloads: 30
XML Downloads: 1364

Web Metrics
Days since publication: 4496
Overall contacts: 55395
Avg. contacts per week: 86.25

Article Citations

Article citations are based on data periodically collected from the Clarivate Web of Science web site
(last update: Feb 2023)

Total number of cites (since 2012): 13
Average cites per year: 1.08

 

Publication Metrics

by Dimensions ©

Articles citing this article

List of the papers citing this article based on CrossRef Cited-by.

 
(1)
André F, Jonard M, Ponette Q (2008)
Precipitation water storage capacity in a temperate mixed oak-beech canopy. Hydrological Processes 22 (20): 4130-4141.
CrossRef | Gscholar
(2)
Andressian V (2004)
Waters and forests: from historical controversy to scientific debate. Journal of Hydrology 291: 1-27.
CrossRef | Gscholar
(3)
Borsy Z, Csongor É, Sárkány S, Szabó I (1981)
Phases of blown-sand movements in the North-East part of the Great Hungarian Plain. Acta geographica ac geologica et meteorologica, Debrecina 20: 5-33.
Gscholar
(4)
Bosch JM, Hewlett JD (1982)
A review of catchment experiments to determine the effect of vegetation changes on water yield and evapotranspiration. Journal of Hydrology 55: 3-23.
CrossRef | Gscholar
(5)
Brutsaert W (1982)
Evaporation into the atmosphere: theory, history, and applications. D. Reidel, Hingham MA, USA, pp. 299.
Gscholar
(6)
Cardon GE, Letey J (1992)
Plant water uptake terms evaluated for soil water and solute movement models. Soil Science Society of America Journal 56 (6): 1876-1880.
CrossRef | Gscholar
(7)
Federer CA, Vörösmarty C, Fekete B (1996)
Intercomparison of methods for calculating potential evaporation in regional and global water balance models. Water Resources Research 32 (7): 2315-2321.
CrossRef | Gscholar
(8)
Federer CA, Vörösmarty C, Fekete B (2003)
Sensitivity of annual evaporation to soil and root properties in two models of contrasting complexity. Journal of Hydrometeorology 4: 1276-1290.
CrossRef | Gscholar
(9)
Gash JHC (1979)
An analytical model of rainfall interception by forests. Quarterly Journal of the Royal Meteorological Society 105: 43-45.
CrossRef | Gscholar
(10)
Gálos B, Lorenz PH, Jacob D (2007)
Will dry events occur more often in Hungary in the future? Environmental Research Letters 2: 034006.
CrossRef | Gscholar
(11)
Green TR, Taniguchi M, Kooi H, Gurdak JJ, Allen DM, Hiscock KM, Treidel H, Aureli A (2011)
Beneath the surface of global change: Impacts of climate change on groundwater. Journal of Hydrology 405: 532-560.
CrossRef | Gscholar
(12)
Gribovszki Z, Kalicz P, Szilágyi J, Kucsara M (2008)
Riparian zone evapotranspiration estimation from diurnal groundwater level fluctuations. Journal of Hydrology 349: 6-17.
CrossRef | Gscholar
(13)
Gribovszki Z, Szilagyi J, Kalicz P (2010)
Diurnal fluctuations in shallow groundwater levels and streamflow rates and their interpretation - A review. Journal of Hydrology 385 (1-4): 371-383.
CrossRef | Gscholar
(14)
IPCC (2007)
Climate change 2007: synthesis report. Contribution of Working Groups I, II and III to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change, Geneva, Switzerland.
Gscholar
(15)
Jarvis PG (1976)
The interpretation of the variations in leaf water potential and stomatal conductance found in canopies in the field. Phil Trans Royal Soc Lond B 273 (927): 593-610.
CrossRef | Gscholar
(16)
Justice CO, Townshend JRG, Vermote EF, Masuoka E, Wolfe RE, El-Saleous N, et al. (2002)
An overview of MODIS land data processing and product status. Remote Sensing of Environment 83: 3-15.
CrossRef | Gscholar
(17)
Kondratiev KY (1969)
Radiation in the atmosphere. Academic Press, New York, USA.
Gscholar
(18)
Ladekarl UL, Rasmussen KR, Christensen S, Jensen KH, Hansen B (2005)
Groundwater recharge and evapotranspiration for two natural ecosystems covered with oak and heather. Journal of Hydrology 300: 76-99.
CrossRef | Gscholar
(19)
Larcher W (1994)
Ökophysiologie der Pflanzen. Verlag Eugen Ulmer, Stuttgart, Germany.
Gscholar
(20)
Lohammar T, Larsson L, Linder S, Falk SO (1980)
FAST - simulation models of gaseous exchange in Scots pine. In: “Structure and function of northern coniferous forests” (Persson T ed). Ecological Bulletins 32: 505-523.
Gscholar
(21)
Loheide II SP, Butler JJ, Gorelick SM (2005)
Estimation of groundwater consumption by phreatophytes using diurnal water table fluctuations: a saturated-unsaturated flow assessment. Water Resources Research 41: W07030.
CrossRef | Gscholar
(22)
Maitre DCL, Scott DF, Colvin C (1999)
A review of information on interactions between vegetation and groundwater. Water South Africa 25: 137-152.
Online | Gscholar
(23)
Menzel L (1997)
Modellierung der Evapotranspiration im System Boden-Pflanze-Atmosphäre. Züricher Geographische Schriften, Heft 67, Geographisches Institut ETH, Zürich, Switzerland, pp. 128.
Gscholar
(24)
Meyboom P (1967)
Groundwater studies in the Assiniboine River drainage basin-part II: hydrologic characteristics of phreatophytic vegetation in south-central Saskatchewan. Bull. Geol. Surv. Can. 139.
Gscholar
(25)
Monteith JL (1965)
Evaporation and environment. In: “The state and movement of water in living organisms” (Fogg GE ed). 19th Symp. Soc. Exp. Biol. Cambridge, UK. The Company of Biologists, pp. 205-234.
Gscholar
(26)
Móricz N (2010)
Water balance study of a groundwater-dependent oak forest. Acta Silvatica & Lignaria Hungarica 6: 49-66.
Online | Gscholar
(27)
Nachabe M, Shah N, Ross M, Vomacka J (2005)
Evapotranspiration of two vegetation covers in a shallow water table environment. Soil Science Society of America Journal 69: 492-499.
CrossRef | Gscholar
(28)
National Forest Inventory Database (2000)
National Forest Inventory Database. Ministry of Rural Development, Budapest, Hungary.
Gscholar
(29)
Otto HJ (1994)
Waldokologie. UTB, Stuttgart, Germany.
Gscholar
(30)
Rawls WJ, Giménez D, Grossman R (1998)
Use of soil texture, bulk density, and the slope of the water retention curve to predict saturated hydraulic conductivity. Transactions American Society of Agricultural Engineers 41 (4): 983-988.
Gscholar
(31)
Ritchie JT (1972)
Model for predicting evaporation from a row crop with incomplete cover. Water Resources Research 8: 1204-1213.
CrossRef | Gscholar
(32)
Roberts J, Rosier P (2005)
The impact of broadleaved woodland on water resources in lowland UK. I. Soil water changes below beech woodland and grass on chalk sites in Hampshire. Hydrology and Earth System Sciences 9 (6): 596-606.
CrossRef | Gscholar
(33)
Schilling KE (2007)
Water table fluctuations under three riparian land covers, Iowa (USA). Hydrological Processes 21: 2415-2424.
CrossRef | Gscholar
(34)
Simunek J, van Genuchten MT, Sejna M (2005)
The Hydrus-1D software package for simulating the one-dimensional movement of water, heat, and multiple solutes in variably-saturated media. Version 3.0, HYDRUS Software Series 1, Department of Environmental Sciences, University of California, Riverside, CA, USA, pp. 270.
Gscholar
(35)
Steyaert LT, Knox RG (2008)
Reconstructed historical land cover and biophysical parameters for studies of land-atmosphere interactions within the eastern United States. Journal of Geophysical Research 113: D02101, pp. 27.
CrossRef | Gscholar
(36)
Stewart JB (1988)
Modelling surface conductance of pine forest. Agricultural and Forest Meteorology 43 (1): 19-35.
CrossRef | Gscholar
(37)
Valente F, David JS, Gash JHC (1997)
Modelling interception loss for two sparse eucalypt and pine forests in central Portugal using reformulated Rutter and Gash analytical models. Journal of Hydrology 190: 141-162.
CrossRef | Gscholar
(38)
van Genucthen MT (1980)
A closed-form equation for predicting the hydraulic conductivity of unsaturated soils. Soil Science Society of America Journal 44: 892-898.
CrossRef | Gscholar
(39)
van Genuchten MT (1987)
A numerical model for water and solute movement in and below the root zone. Research Report No 121, U.S. Salinity Laboratory, USDA, ARS, Riverside, California, USA, pp. 221.
Gscholar
(40)
van Genuchten MT, Leij FJ, Yates SR (1991)
The RETC code for quantifying the hydraulic functions of unsaturated soils, Version 1.0. EPA Report 600/2-91/065, U.S. Salinity Laboratory, USDA, ARS, Riverside, California, USA, pp. 93.
Gscholar
(41)
von Hoyningen-Hüne J (1983)
Die Interception des Niederschlags in landwirtschaftlichen Beständen. Schriftenreihe des DVWK 57: 1-53.
Gscholar
(42)
Wang Q, Adiku S, Tenhunen J, Granier A (2005)
On the relationship of NDVI with leaf area index in a decidiouos forest site. Remote Sensing of Environment 94: 244-255.
CrossRef | Gscholar
(43)
Wattenbach M, Hattermann F, Weng R, Wechsung F, Krysanova V, Badeck F (2005)
A simplified approach to implement forest eco-hydrological properties in regional hydrological modeling. Ecological Modelling 187: 40-59.
CrossRef | Gscholar
(44)
White WN (1932)
Method of estimating groundwater supplies based on discharge by plants and evaporation from soil - results of investigation in Escalante Valley, Utah. US Geological Survey, Water Supply Paper 659-A: 1-105.
Gscholar
 

This website uses cookies to ensure you get the best experience on our website. More info