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Books on the topic 'Soil-water balance'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 March 2023

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1

International Crops Research Institute for the Semi-arid Tropics. and International Workshop on Soil Water Balance inthe Sudano-Sahelian Zone (1991 : Niamey, Niger), eds. Soil water balance in the Sudano-Sahelian zone: Summary proceedings of an International Workshop on soil water ... 18-23 Feb 1991 Niamey, Niger. Patancheru: International Crops Research Institute for the Semi-arid Tropics,India, 1992.

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2

Westenbroek, Stephen M. SWB--a modified Thornthwaite-Mather Soil-Water-Balance code for estimating groundwater recharge. Reston, Va: U.S. Dept. of the Interior, U.S. Geological Survey, Ground Resources Program, 2010.

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3

Dumouchelle, D. H. Evaluation of ground-water/surface-water relations, Chapman Creek, west-central Ohio, by means of multiple methods. Columbus, OH: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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4

Dumouchelle, D. H. Evaluation of ground-water/surface-water relations, Chapman Creek, west-central Ohio, by means of multiple methods. Columbus, Ohio: U.S. Dept. of the Interior, U.S. Geological Survey, 2001.

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5

Bidlake, W. R. Simulation of the soil water balance of an undeveloped prairie in west-central Florida. Washington, DC: U.S. G.P.O., 1997.

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6

Boer, M. Assessment of dryland degradation: Linking theory and practice through site water balance modelling. Utrecht: Koninklijk Nederlands Aardrijkskundig Genootschap/Faculteit Ruimtelijke Wetenschappen Universiteit Utrecht, 1999.

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7

Small, Eric E. The influence of soil moisture on the surface energy balance in semiarid environments. Las Cruces, N.M: New Mexico Water Resources Research Institute, New Mexico State University, 2001.

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8

Zimmermann, Lothar. Der Bodenwasserhaushalt an einem Hochlagenstandort im Südschwarzwald. Freiburg im Breisgau: Institut für Bodenkunde und Waldernährungslehre der Albert-Ludwigs-Universität Freiburg i.Br., 1995.

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9

Kirsten, Verburg, and CSIRO (Australia). Division of Soils., eds. Methodology in soil water and solute balance modelling: An evaluation of the APSIM-SoilWat and SWIMv2 models : report of an APSRU/CSIRO Division of Soils workshop held in Brisbane, Australia, 16-18 May 1995. [Australia]: CSIRO Australia, Division of Soils, 1996.

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10

Rex, John F. Hydrologic effects of mountain pine beetle infestation and salvage-harvesting operations. Victoria, B.C: Pacific Forestry Centre, 2009.

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11

International Conference Soils and the Greenhouse Effect (1989 Wageningen, Netherlands). Soils and the greenhouse effect: The present status and future trends concerning the effect of soils and their cover on the fluxes of greenhouse gases, the surface energy balance, and the water balance : proceedings of the International Conference Soils and the Greenhouse Effect. Chichester: Wiley, 1990.

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12

Soil water balance in the Sudano-Sahelian zone. Wallingford, Oxfordshire, UK: International Association of Hydrological Sciences, 1991.

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13

Reece, Clive Frank. Sparse plant community effects on soil water balance of an arid site. 1991.

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14

Zhang, L., GR Walker, and M. Fleming. Surface Water Balance for Recharge Estimation - Part 9. CSIRO Publishing, 2002. http://dx.doi.org/10.1071/9780643105416.

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This addition to The Basics of Recharge and Discharge series deals with the surface water balance approaches that form the traditional basis of hydrological investigations. It explores both field methods and modelling methods for measuring or estimating the different parts of the water balance, including rainfall, evaporation, run-off and soil water storage. The authors discuss the concepts required to understand a surface water balance result or to set up an experiment. As water balance studies can be both time-consuming and expensive, this report will give readers a better understanding of water balance approaches and the considerations before going into a water balance study for the purpose of deep drainage.

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15

Grayson, Susana Maria. Automated water balance procedure for large-scale experimental databases based on soil moisture. 1996.

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16

Carrijo, Osmar Alves. Analysis of a hydrologic balance model and Penman-Monteith evapotranspiration estimating methods. 1988.

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17

Kacorzyk, Piotr. Wartość gospodarcza okrywy roślinnej gleby w aspekcie nawożenia oraz zdolności retencyjnej płytki gleby górskiej. Publishing House of the University of Agriculture in Krakow, 2018. http://dx.doi.org/10.15576/978-83-66602-33-5.

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The aim of the study was to assess the impact of method management of mountain soil on the quantity and quality of waste water, and the amount of mineral nutrients it contains. I have analyzed the water, that was moved through the soil profiles of 0-20 cm and 0-40 cm depth. I have also evaluated the floristic composition, the productivity of grassland and arable land, and the use of fertilizers by vegetation and soil chemical properties. I have found that the type of plant cover of the soil had a significant effect on the amount and chemical composition of water moving through the soil profile. Arable land was characterized by an average of 5 percentage point higher drainage rates compared to meadows. The smallest outflow of water from the soil was found in the first research period (intensive vegetation), and the largest in the third period (non-vegetation). The largest amount of the mineral content carried out annually with a soaking water, was observed on the arable land and was on average more than 2 times larger than on other fertilizers. This evidenced by the greater variation in the composition of floristic vegetation and its productivity. Between 0-20 cm and 0-40 cm of soil profiles, significant differences in the amount of waste water and mineral components were observed. The water drainage coefficient from the shallow profile was on average 9 percentage points higher than from the deeper profile. The amount of the sum of mineral loads, excluding calcium from the shallow soil profile was 94,5% higher than the sum of loads taken from the deeper soil profile. In the unused meadow the improvement of soil chemical properties was observed. There was an increase in pH, and the accumulation of minerals resulted from the positive balance of most of the ingredients.

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18

Sivakumar, M. V. K., J. S. Wallace, C. Renard, and C. Giroux. Series of Proceedings and Reports: Soil Water Balance in the Sudano-Sahelian Zone -Proceedings of a Workshop Held at Niamey (Niger), February 1991 (Series of Proceedings and Reports). IAHS Press, 1991.

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19

Water Balance Covers for Waste Containment Principles and Practice. American Society of Civil Engineers, 2010.

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20

Payne, Cymie R. Developments in the Law of Environmental Reparations. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198784630.003.0015.

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The United Nations Compensation Commission (‘UNCC’) is a unique model for liability and compensation of environmental damage in an international context, influencing both jus in bello and jus post bellum. The UNCC provided a legal process that catalogued, assessed, and awarded money to pay to clean and repair the damaged soil, water, coastal ecosystems, and other harms resulting from the 1990–1 Gulf War. Its contributions include integration of environmental law principles into the reparations process; use of advanced techniques for assessment of environmental damage; and use of a multilateral process in a way that balanced confidentiality and transparency. The UNCC environmental programme, viewed as an innovative approach to justice after war, highlights the contribution that the environmental integrity norm can make.

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