Relevant bibliographies by topics / Soil and Water Sciences

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Soil and Water Sciences'

Author: Grafiati
Published: 4 June 2021
Last updated: 20 February 2023

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Journal articles on the topic "Soil and Water Sciences"

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Raats, P. A. C. "Applications of material coordinates in the soil and plant sciences." Netherlands Journal of Agricultural Science 35, no. 3 (August 1, 1987): 361–70. http://dx.doi.org/10.18174/njas.v35i3.16731.

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The continuum theory of mixtures is used to show the common basis of models in three areas. In each, the central problem is the description of the deformation and motion of a reference continuum and of the movement of one or more constituents relative to this reference continuum. The three applications concern the movement of solutes relative to soil water, the movement of soil water relative to the solid phase of swelling/shrinking soils, and the movement of water, solutes, and gases relative to growing plant tissues. (Abstract retrieved from CAB Abstracts by CABI’s permission)
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Thomas, R. L. "Soil and water science." Soil and Tillage Research 42, no. 1-2 (May 1997): 141–42. http://dx.doi.org/10.1016/s0167-1987(97)83358-2.

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Kroulík, M., J. Hůla, R. Šindelář, and F. Illek. "Water infiltration into soil related to the soil tillage intensity." Soil and Water Research 2, No. 1 (January 7, 2008): 15–24. http://dx.doi.org/10.17221/2098-swr.

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Soil infiltration capacity is one of the key factors in the soil protection against unfavourable effects of water erosion. The purpose of its measuring was to compare and evaluate the changes of the soil physical properties and of water infiltration into soil caused by different intensity of soil cultivation at two individual sites. The ploughing (PL), shallow tillage (ST), and direct drilling (NT) effects on the soil physical properties, water infiltration into soil, and soil surface coverage with the crop residua under the soil condition loamy Haplic Luvisol, with long-term growing of maize
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Ende, J. van den. "Water contents of glasshouse soils at field capacity and at saturation. 1. Relationships between water contents." Netherlands Journal of Agricultural Science 36, no. 3 (August 1, 1988): 265–74. http://dx.doi.org/10.18174/njas.v36i3.16678.

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The relationship between water contents at saturation and at field capacity was determined in soils from 75 glasshouses in the Netherlands. Sandy, loamy and peaty soils were equally represented. Water contents of soils at sampling time were found to correspond closely with those at field capacity. Water contents of saturated pastes obtained from field-moist soil samples were higher than those of saturated pastes obtained from soil samples dried previously. For the relationships between water contents of field-moist soil samples and of saturated pastes obtained from field-moist and dried soil s
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Bouma, Johan. "Soil Security in Sustainable Development." Soil Systems 3, no. 1 (January 8, 2019): 5. http://dx.doi.org/10.3390/soilsystems3010005.

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The United Nations (UN) Sustainable Development Goals (SDGs) provide an excellent channel to demonstrate the significance of soils when considering e.g., food production, water availability, climate mitigation and biodiversity preservation. For environmental sciences, including soil science, the SDGs provide “a point at the horizon” for future research. Progress to achieve the SDGs by 2030 will bureaucratically be monitored by targets and indicators but questions as to how effective research should be organized remain unanswered so far. The soil security concept, based on the five Cs (capabili
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Brillante, L., O. Mathieu, B. Bois, C. van Leeuwen, and J. Lévêque. "The use of soil electrical resistivity to monitor plant and soil water relationships in vineyards." SOIL 1, no. 1 (March 17, 2015): 273–86. http://dx.doi.org/10.5194/soil-1-273-2015.

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Abstract. Soil water availability deeply affects plant physiology. In viticulture it is considered a major contributor to the "terroir" effect. The assessment of soil water in field conditions is a difficult task, especially over large surfaces. New techniques are therefore required in order to better explore variations of soil water content in space and time with low disturbance and with great precision. Electrical resistivity tomography (ERT) meets these requirements for applications in plant sciences, agriculture and ecology. In this paper, possible techniques to develop models that allow t
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Pierzgalski, Edward, and Jerzy Jeznach. "Measures for soil water control in Poland." Journal of Water and Land Development 10, no. 1 (December 1, 2006): 79–89. http://dx.doi.org/10.2478/v10025-007-0007-5.

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Measures for soil water control in Poland Polish water resources depend on precipitations, which are variable in time and space. In dry years the water balance is negative in central parts of Poland but sudden thaws and downfalls may result in periodical water excess and dangerous floods almost in the entire country. The retention capacity of artificial reservoirs in Poland permits to store only 6% of the average annual runoff, which is commonly considered insufficient. Another method to increase retention is soil water control. About fifty percent of soils in Poland consist of light and very
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Judy, Jonathan D., Maria L. Silveira, Sampson Agyin-Birikorang, George O'Connor, and Thomas A. Obreza. "Drinking Water Treatment Residuals to Control Phosphorus in Soils." EDIS 2019 (August 21, 2019): 6. http://dx.doi.org/10.32473/edis-ss513-2019.

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Soils in Florida may contain excess soil phosphorus (P) resulting from fertilizer, manure or biosolids applications. Excess P in soil does not damage soil fertility but can be transported from agricultural and urban areas either dissolved in water that drains away or as particulate matter (attached to soil particles) that travels with eroding soil. Increased P in water bodies is recognized as one of the major factors responsible for eutrophication-related decrease in water quality. Most soils have the capacity to retain excess P. However, soils with low capacity to retain excess P are abundant
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de Jonge, Lis W., Per Moldrup, and Ole H. Jacobsen. "SOIL-WATER CONTENT DEPENDENCY OF WATER REPELLENCY IN SOILS." Soil Science 172, no. 8 (August 2007): 577–88. http://dx.doi.org/10.1097/ss.0b013e318065c090.

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Wang, Xiaofang, Yi Li, Yichen Wang, and Chuncheng Liu. "Performance of HYDRUS-1D for simulating water movement in water-repellent soils." Canadian Journal of Soil Science 98, no. 3 (September 1, 2018): 407–20. http://dx.doi.org/10.1139/cjss-2017-0116.

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Soil water repellency affects soil water movement during infiltration significantly. The HYDRUS software has been popularly applied in soil water dynamics simulation for many years, but its performance in water-repellent (WR) soils has not been assessed thoroughly. Our objectives are to assess the performance of HYDRYUS-1D for cumulative infiltration (CI), wetting front (Zf), and volumetric soil water content (θv) during horizontal imbibition and vertical infiltration in wettable, slightly WR, and strongly WR soils. The key parameters of α and n in water retention curves were inversely estimat
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Dissertations / Theses on the topic "Soil and Water Sciences"

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Ekanayake, Jagath C. "Soil water movement through swelling soils." Lincoln University, 1990. http://hdl.handle.net/10182/1761.

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The present work is a contribution to description and understanding of the distribution and movement of water in swelling soils. In order to investigate the moisture distribution in swelling soils a detailed knowledge of volume change properties, flow characteristics and total potential of water in the soil is essential. Therefore, a possible volume change mechanism is first described by dividing the swelling soils into four categories and volume change of a swelling soil is measured under different overburden pressures. The measured and calculated (from volume change data) overburden potentia
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Poon, David. "Re-conceptualizing the soil and water assessment tool to better predict subsurface water flow through macroporous soils." Thesis, McGill University, 2013. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=119707.

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Efforts to manage eutrophication of surface waters should recognize that macropore flow transports significantly more phosphorus (P) to surface waters via tile drains than water that percolates through the soil matrix. For the watershed-scale SWAT (Soil and Water Assessment Tool) model to describe phosphorus transport through tile drains, SWAT needs to partition percolation into macropore flow and matrix flow. The objective of this study was to evaluate the effects of a new macropore flow algorithm on the partitioning of hydrological flows, using input data that are readily available, consiste
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Subedi-Chalise, Kopila. "Impacts of Crop Residue and Cover Crops on Soil Hydrological Properties, Soil Water Storage and Water Use Efficiency of Soybean Crop." Thesis, South Dakota State University, 2017. http://pqdtopen.proquest.com/#viewpdf?dispub=10265200.

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<p> Cover crops and crop residue play a multifunctional role in improving soil hydrological properties, soil water storage and water use efficiency (WUE). This study was conducted to better understand the role of crop residue and cover crop on soil properties and soil water dynamics. The study was conducted at the USDA-ARS North Central Agricultural Research Laboratory, located in Brookings, South Dakota. Two residue removal treatments that include low residue removal (LRR) and high residue removal (HRR) were established in 2000 with randomized complete block design under no-till corn (Zea may
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Dryden, Garri A. "Optimum gravel size for use as a soil surface cover for the prevention of soil erosion by water." Diss., The University of Arizona, 2003. http://hdl.handle.net/10150/280469.

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Eleven series of replicated tests were conducted using 38.1 mm, 15.9 mm, and 9.5 mm gravel to determine the most effective soil surface cover to prevent soil erosion from rainfall. A sediment tray one meter square in size with an integrated rainfall simulator was used to generate data after initial trial runs had established test procedures. Various size gravels and a control with no cover were tested in a laboratory using simulated rainfall to evaluate their effectiveness in preventing erosion. Through thirty-three experiments, signature traits of specific rock sizes were identified. Experime
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Shahadha, Saadi Sattar. "Measured Soil Hydraulic Properties as RZWQM2 Input to Simulate Soil Water Dynamics and Crop Evapotranspiration." UKnowledge, 2018. https://uknowledge.uky.edu/pss_etds/110.

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Agricultural system models integrate many different processes that cannot all be measured in field experiments and help quantify soil water dynamics, crop evapotranspiration, and crop growth with high temporal resolution. Understanding soil water dynamics and crop evapotranspiration is essential to improve agricultural management of field crops. For example, the interaction between nitrogen application rate and water dynamics is not sufficiently understood. In most cases, model simulations deviate from field measurements, especially when model input parameters are indirectly and unspecifically
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Undercoffer, Jason. "Monitoring Phosphorus Transport and Soil Test Phosphorus From Two Distinct Drinking Water Treatment Residual Application Methods." The Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=osu1243532451.

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Pricope, Narcisa. "Modeling Soil Erosion in the Upper Green River, KY." TopSCHOLAR®, 2006. http://digitalcommons.wku.edu/theses/258.

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Off-site soil erosion has tremendous impacts on the present state of most river systems throughout the United States, contributing sediments to channels mainly as nonpoint pollution resulting from land-use and agricultural practices and leading to sedimentation downstream and downwind, a decrease in the transport capacity of streams, increase in the risk of flooding, filling reservoirs, and eutrophication. A primary focus in examining the problems associated with soil erosion arid ultimately in proposing control measures should be on identifying the sources of the sediment. Therefore, a model
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Zelasko, Amanda Jean. "Soil reduction rates under water saturated conditions in relation to soil properties." NCSU, 2007. http://www.lib.ncsu.edu/theses/available/etd-07172007-154810/.

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The success of wetland restoration projects depends in part on the length of time that a soil is in a reduced redox state. The length of time that a soil is reduced depends on how quickly reduction occurs following saturation with water. The relationship between reduction rate and various soil chemical and mineralogical properties is poorly understood, but such properties might be manipulated to improve the success of wetland restoration projects. The goals of this research were to determine soil properties that predict the rate at which soils undergo reduction when saturated, and to determine
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LIU, ZHIJUN. "Effective modeling of agricultural practices within large-scale hydrologic and water quality simulations." MSSTATE, 2006. http://sun.library.msstate.edu/ETD-db/theses/available/etd-11082006-162139/.

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The previously developed watershed hydrological and water quality model for St. Louis Bay watershed by Kieffer (2002) was refined and calibrated. The aspects of model development refinement included development of fertilization-related nutrient input parameters, evaluation of nutrient input methods, development of plant uptake-related nutrient input parameters, non-cropland simulation using PQUAL module, and recalibration of hydrology in Jourdan River. The related information of typical cropland management practice based on consultation from Mississippi State University Extention Service perso
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Bastviken, Paulina. "Soil water solution DOC dynamics during winter in boreal hillslopes." Thesis, Uppsala universitet, Institutionen för geovetenskaper, 2014. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-229128.

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When plants and animals die they are decomposed into microscopic particles of organic carbon. In the ground, these carbon particles are dissolved in the soil water and eventually transported to the streamchannel with the flow of the groundwater. Today the quantities of dissolved organic carbon (DOC) have been observed to increase in many lakes and streams around the world, which constitute a threat against the water quality and ecologic environment of these surface waters. The amount of organic carbon that is dissolved and transported in the soil water is mainly controlled by processes related
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Books on the topic "Soil and Water Sciences"

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Vaníček, Ivan. Earth structures: In transport, water and environmental engineering. Dordrecht: Springer, 2008.

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Agency, European Space. SMOS: ESA's water mission. Noordwijk, The Netherlands]: ESA, 2010.

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H, Tunney, ed. Phosphorus loss from soil to water. Wallingford, OX: CAB International, 1997.

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Workshop "Soil and Water Quality at Different Scales" (1996 Wageningen, Netherlands). Soil and water quality at different scales: Proceedings of the Workshop "Soil and Water Quality at Different Scales", held 7-9 August 1996, Wageningen, The Netherlands. Dordrecht: Kluwer Academic Publishers, 1998.

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Donahue, Roy Luther. Our soils and their management: Increasing production through environmental soil and water conservation and fertility management. 6th ed. Danville, Ill: Interstate Publishers, 1990.

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Environmental soil and water chemistry: Principles and applications. New York: Wiley, 1998.

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L, Davis Susan, Pyke Grantley W, Reinhart Jill M, Scanlon Karen A, Conservation Technology Information Center, and AWWA Research Foundation, eds. Water utility/agricultural alliances: Working together for cleaner water. Denver, CO: AWWA Research Foundation and American Water Works Association, 2005.

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Conference on Contaminated soils (19th 2003 University of Massachusetts, Amherst). Contaminated soils, sediments, and water, volume 9: Science in the real world. New York: Springer, 2005.

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Baker, Ralph S., Glendon W. Gee, and Cynthia Rosenzweig, eds. Soil and Water Science: Key to Understanding Our Global Environment. Madison, WI, USA: Soil Science Society of America, 1994. http://dx.doi.org/10.2136/sssaspecpub41.

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Ian, Cordery, Iacovides Iacovos, and SpringerLink (Online service), eds. Coping with Water Scarcity: Addressing the Challenges. Dordrecht: Springer Netherlands, 2009.

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Book chapters on the topic "Soil and Water Sciences"

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Mukherjee, Swapna. "Soil Water." In Current Topics in Soil Science, 87–104. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-92669-4_9.

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McCool, D. K., and K. G. Renard. "Water Erosion and Water Quality." In Advances in Soil Science, 175–85. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8982-8_8.

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Wallis, M. G., and D. J. Horne. "Soil Water Repellency." In Advances in Soil Science, 91–146. New York, NY: Springer New York, 1992. http://dx.doi.org/10.1007/978-1-4612-2930-8_2.

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Parkin, Gary W., Walter H. Gardner, and K. Auerswald. "Water Erosion." In Encyclopedia of Soil Science, 817–22. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_625.

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Parkin, Gary W., Walter H. Gardner, K. Auerswald, and Johannes Bouma. "Water Movement." In Encyclopedia of Soil Science, 822–25. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_628.

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Ritsema, Coen J., Louis W. Dekker, Klaas Oostindie, Demie Moore, and Bernd Leinauer. "Soil Water Repellency and Critical Soil Water Content." In Soil Science Step-by-Step Field Analysis, 97–112. Madison, WI, USA: American Society of Agronomy and Soil Science Society of America, 2015. http://dx.doi.org/10.2136/2008.soilsciencestepbystep.c8.

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Stewart, B. A., and J. L. Steiner. "Water-Use Efficiency." In Advances in Soil Science, 151–73. New York, NY: Springer New York, 1990. http://dx.doi.org/10.1007/978-1-4613-8982-8_7.

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Paz, Carlota Garcia, Teresa Taboada Rodríguez, Valerie M. Behan‐Pelletier, Stuart B. Hill, Pablo Vidal‐Torrado, Miguel Cooper, Peter van Straaten, et al. "Field Water Cycle." In Encyclopedia of Soil Science, 272–75. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_228.

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Chesworth, Ward, Otto Spaargaren, Amos Hadas, and Pieter H. Groenevelt. "Thermodynamics of Soil Water." In Encyclopedia of Soil Science, 772–76. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_594.

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Parkin, Gary W. "Water Budget In Soil." In Encyclopedia of Soil Science, 811–13. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-3995-9_622.

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Conference papers on the topic "Soil and Water Sciences"

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D'Ambrosio, Roberta, Antonia Longobardi, and Mirka Mobilia. "Evaluation of green-roofs evolution's impact on substrate soil water content by FDR sensors calibration." In 5th International Electronic Conference on Water Sciences. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecws-5-08028.

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Karamouz, Mohammad, Arash Ghomlaghi, Reza Saleh Alipour, Mahta Nazari, and Mohammad Fereshtehpour. "Soil Moisture Data: From Using Citizen Science to Satellite Technology." In World Environmental and Water Resources Congress 2019. Reston, VA: American Society of Civil Engineers, 2019. http://dx.doi.org/10.1061/9780784482322.009.

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Ilie, Ana Maria Carmen, Cody Goebel, and Tissa Illangasekare. "Performance assessment of soil moisture sensors under controlled conditions in laboratory setting and recommendations for field deployment." In 5th International Electronic Conference on Water Sciences. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecws-5-08041.

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Saleh, Ismail, Ida Setya Wahyu Atmaja, and Ray March Syahadat. "Prohibition in Baduy Dalam Community: Soil and Water Conservation Perspective." In International Conference on Agriculture, Social Sciences, Education, Technology and Health (ICASSETH 2019). Paris, France: Atlantis Press, 2020. http://dx.doi.org/10.2991/assehr.k.200402.040.

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Mishra, Ashutosh, Paras Pujari, Shalini Dhyani, and Parikshit Verma. "Soil-water dynamics in flood irrigated orange orchard in central India: Integrated approach of sap flow measurements and HYDRUS 1D model." In 5th International Electronic Conference on Water Sciences. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecws-5-08467.

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Jalut, Qassem H., and Anmar S. Saleh. "Evaluation of conjunctive water use impacts on soil hydraulic properties and root water uptake using HYDRUS-3D model." In 2018 1st- International Scientific Conference of Engineering Sciences - 3rd Scientific Conference of Engineering Science (ISCES). IEEE, 2018. http://dx.doi.org/10.1109/isces.2018.8340564.

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Abdullah, N. H. H., N. W. Kuan, A. Ibrahim, B. N. Ismail, M. R. A. Majid, R. Ramli, and N. S. Mansor. "Determination of soil water content using time domain reflectometer (TDR) for clayey soil." In ADVANCES IN CIVIL ENGINEERING AND SCIENCE TECHNOLOGY. Author(s), 2018. http://dx.doi.org/10.1063/1.5062642.

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AKINYINKA, AKINNUSOTU, Justinah Ukpebor, and Felix Okiemen. "Assessment of polycyclic aromatic hydrocarbons (PAHs) in sediment and fish samples of river Owan, and agricultural soil around the same river in Edo State, Nigeria." In 5th International Electronic Conference on Water Sciences. Basel, Switzerland: MDPI, 2020. http://dx.doi.org/10.3390/ecws-5-08447.

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Mukhlisin, Muhammad, Marlin Ramadhan Baidillah, and Mohd Raihan Taha. "Electrical Capacitance Volume Tomography (ECVT) for Measurement Soil Water Infiltration in Vessel Experiments." In 1st Annual International Conference on Geological & Earth Sciences. Global Science Technology Forum, 2012. http://dx.doi.org/10.5176/2251-3361_geos12.113.

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Talapessy, Ronaldo, and Oktaviana K. Sujianti. "A simple technique to investigate water flow in soil based on electrical waveform." In THE 7TH INTERNATIONAL CONFERENCE ON BASIC SCIENCES 2021 (ICBS 2021). AIP Publishing, 2023. http://dx.doi.org/10.1063/5.0112532.

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Reports on the topic "Soil and Water Sciences"

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Beal, Samuel, Ashley Mossell, and Jay Clausen. Hydrocarbon treatability study of Antarctica soil with Fenton’s reagent. Engineer Research and Development Center (U.S.), July 2021. http://dx.doi.org/10.21079/11681/41260.

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The study objectives were to determine the effectiveness of Fenton’s Reagent and Modified Fenton’s Reagent in reducing Total Petroleum Hydrocarbon (TPH) concentrations in petroleum-contaminated soil from McMurdo Station, Antarctica. Comparisons of the contaminated soils were made, and a treatability study was completed and documented. This material was presented at the Association for Environmental Health and Sciences Foundation (AEHS) 30th Annual International Conference on Soil, Water, Energy, and Air (Virtual) on March 25, 2021.
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Gillor, Osnat, Stefan Wuertz, Karen Shapiro, Nirit Bernstein, Woutrina Miller, Patricia Conrad, and Moshe Herzberg. Science-Based Monitoring for Produce Safety: Comparing Indicators and Pathogens in Water, Soil, and Crops. United States Department of Agriculture, May 2013. http://dx.doi.org/10.32747/2013.7613884.bard.

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Using treated wastewater (TWW) for crop irrigation represents an important opportunity for ensuring adequate food production in light of growing freshwater scarcity worldwide. However, the environmentally sustainable approach of using TWW for irrigation can lead to contamination of produce with fecal pathogens that may remain in treated water. The overall goal of this research was to evaluate the correlation between the presence of fecal indicator bacteria (FIB) and that of a suite of human pathogens in TWW, the irrigated soil, and crops. Field experiments were conducted to compare secondary a
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David, Gabrielle C. L., Patrick H. Trier, Ken M. Fritz, Steven L. Kichefski, Tracie-Lynn Nadeau, L. Allan James, Brian J. Topping, Wohl Ellen E., and Aaron Allen. National Ordinary High Water Mark Field Delineation Manual for Rivers and Streams : Interim Version. U.S. Army Engineer Reseach and Development Center, November 2022. http://dx.doi.org/10.21079/11681/46102.

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The ordinary high water mark (OHWM) defines the lateral extent of nontidal aquatic features in the absence of adjacent wetlands in the United States. The federal regulatory definition of the OHWM, 33 CFR 328.3(c)(7), states the OHWM is “that line on the shore established by the fluctuations of water and indicated by physical characteristics such as [a] clear, natural line impressed on the bank, shelving, changes in the character of soil, destruction of terrestrial vegetation, the presence of litter and debris, or other appropriate means that consider the characteristics of the surrounding area
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Stevens A. J. Booster soil, component, and water activation. Office of Scientific and Technical Information (OSTI), September 1987. http://dx.doi.org/10.2172/1150470.

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Jayaweera, Indira S., Montserrat Marti-Perez, Jordi Diaz-Ferrero, and Angel Sanjurjo. Water as a Reagent for Soil Remediation. Office of Scientific and Technical Information (OSTI), March 2003. http://dx.doi.org/10.2172/808528.

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Indira S. Jayaweera, Montserrat Marti-Perez, Jordi Diaz-Ferrero, and Angel Sanjurjo. WATER AS A REAGENT FOR SOIL REMEDIATION. Office of Scientific and Technical Information (OSTI), November 2001. http://dx.doi.org/10.2172/808964.

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Atalay, A., and D. Vir Maggon. Selenium in Oklahoma ground water and soil. Office of Scientific and Technical Information (OSTI), March 1991. http://dx.doi.org/10.2172/5127191.

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Indira S. Jayaweera, Montserrat Marti-Perez, Jordi Diaz-Ferrero, and Angel Sanjurjo. WATER AS A REAGENT FOR SOIL REMEDIATION. Office of Scientific and Technical Information (OSTI), March 2001. http://dx.doi.org/10.2172/824937.

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Indira S. Jayaweera and Jordi Diaz-Ferraro. WATER AS A REAGENT FOR SOIL REMEDIATION. Office of Scientific and Technical Information (OSTI), February 2000. http://dx.doi.org/10.2172/824939.

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Krajewski, W., H. Loesche, R. Mason, K. McGuire, B. Mohanty, G. Poulos, P. Reed, J. Shanley, O. Wendroth, and D. A. Robinson. Enhanced Water Cycle Measurements for Watershed Hydrologic Sciences Research. Chair J. Jacobs. Consortium of Universities for the Advancement of Hydrologic Science, Inc. (CUAHSI), May 2006. http://dx.doi.org/10.4211/techrpts.200605.wc.

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You might also be interested in the extended bibliographies on the topic 'Soil and Water Sciences' for particular source types:
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