Boron Toxicity and Deficiency in Agricultural Plants
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Cultivation of Soils for Forestry
Forestry Commission ARCHIVE Forestry Commission Bulletin 119 Cultivation of Soils for Forestry FORESTRY COMMISSION BULLETIN 119 Cultivation of Soils for Forestry D.B. Paterson and W. L. Mason Forest Research, Silviculture North Branch, Northern Research Station, Roslin, Midlothian EH25 9SY Forestry Commission, Edinburgh © Crown copyright 1999 Applications for reproduction should he made to HMSO, The Copyright Unit St Clements House, 2-16 Colegate, Norwich NR3 1BQ ISBN 0 85538 400 X Paterson, David B. and Mason, William L., 1999. Cultivation of Soils for Forestry. Bulletin 119. FDC 237:114:(410) KEYWORDS: Forestry, Cultivation, Soils Acknowledgements Special thanks are due to Chris Quine, Silviculturist at Northern Research Station, who made available his unpublished Cultivation Review and many background papers and references. We thank the project leaders, research foresters and workers, past and present in Silviculture (North), and the former Site Studies and Physiology Branches who initiated and managed the experiments reported here and gave permission for their results to be used. The statistical services of I.M.S. White are gratefully acknowledged. The reports of Technical Development Branch (formerly Work Study) on trials of cultivation machinery have been heavily used. Many authors outside the Forestry Commission have provided valuable information - with particular thanks to R. Schaible, M. Carey and E. Hendrick in Ireland and D.C. Malcolm of Edinburgh University. Numerous helpful comments have been made by Graham Pyatt, Richard Toleman, John Morgan, Duncan Ray, David Henderson- Howat and Brian Spencer. Karen Chambers edited and substantially improved the structure and presentation of an early draft. Finally, we are grateful to Madge Holmes for typing various drafts, Glenn Brearley for illustrations and John Parker for editorial and publishing services. -
Trace Elements and Minerals in Fumarolic Sulfur: the Case of Ebeko Volcano, Kuriles
Hindawi Geofluids Volume 2018, Article ID 4586363, 16 pages https://doi.org/10.1155/2018/4586363 Research Article Trace Elements and Minerals in Fumarolic Sulfur: The Case of Ebeko Volcano, Kuriles E. P. Shevko,1 S. B. Bortnikova,2 N. A. Abrosimova,2 V. S. Kamenetsky ,3,4 S. P. Bortnikova,2 G. L. Panin,2 and M. Zelenski 3 1 Sobolev Institute of Geology and Mineralogy, SBRAS, Novosibirsk 630090, Russia 2Trofmuk Institute of Petroleum Geology and Geophysics, SBRAS, No. 3, Novosibirsk 630090, Russia 3Institute of Experimental Mineralogy RAS, Chernogolovka 142432, Russia 4EarthSciencesandCODES,UniversityofTasmania,PrivateBag79,Hobart,TAS7001,Australia Correspondence should be addressed to M. Zelenski; [email protected] Received 25 June 2017; Revised 13 October 2017; Accepted 14 December 2017; Published 20 March 2018 Academic Editor: Joerg Goettlicher Copyright © 2018 E. P. Shevko et al. Tis is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited. Native sulfur deposits on fumarolic felds at Ebeko volcano (Northern Kuriles, Russia) are enriched in chalcophile elements (As- Sb-Se-Te-Hg-Cu) and contain rare heavy metal sulfdes (Ag2S, HgS, and CuS), native metal alloys (Au2Pd), and some other low- solubility minerals (CaWO4, BaSO4). Sulfur incrustations are impregnated with numerous particles of fresh and altered andesite groundmass and phenocrysts (pyroxene, magnetite) as well as secondary minerals, such as opal, alunite, and abundant octahedral pyrite crystals. Te comparison of elemental abundances in sulfur and unaltered rocks (andesite) demonstrated that rock-forming elements (Ca, K, Fe, Mn, and Ti) and other lithophile and chalcophile elements are mainly transported by fumarolic gas as aerosol particles, whereas semimetals (As, Sb, Se, and Te), halogens (Br and I), and Hg are likely transported as volatile species, even ∘ at temperatures slightly above 100 C. -
Soils and Their Main Characteristics
Higher Geography Physical Environments Biosphere Soils Higher Geography course The 3 types of soil studied as part of the Higher Geography course are: • Brown Earths •Podzols •Gleys Characteristics of Brown Earths • Free draining • Brown/reddish brown • Deciduous woodland • Litter rich in nutrients • Intense biological activity e.g. earthworms • Mull humus Brown Earth Profile • Ah-topsoil dark coloured enriched with mull humus, variable depth • B - subsoil with distinctive brown/red brown colours • Lightening in colour as organic matter/iron content decreases with depth Brown Earth: Soil forming factors • Parent material • Variable soil texture •Climate • Relatively warm, dry • Vegetation/organisms • Broadleaf woodland, mull humus, indistinct horizons • Rapid decomposition • Often earthworms and other mixers • Topography • Generally low lying •Time • Since end of last ice age c10,000 years Organisms in Brown Earths False colour SEM of mixture of soil fungi and bacteria Help create a good and well aggregated, aerated and fertile crumb structured soil Thin section of soil showing enchytraeid faecal material Earthworm activity is important in soil mixing Uses of Brown Earths • Amongst the most fertile soils in Scotland • Used extensively for agriculture e.g. winter vegetables • Fertilisers required to maintain nutrient levels under agriculture • Occurring on gently undulating terrain - used extensively for settlement and industry • Sheltered sites suit growth of trees Test yourself: Brown Earths Write down 3 characteristics of a brown earth -
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Geochemical Journal, Vol. 41, pp. 149 to 163, 2007 Boron isotope fractionation accompanying formation of potassium, sodium and lithium borates from boron-bearing solutions MAMORU YAMAHIRA, YOSHIKAZU KIKAWADA* and TAKAO OI Department of Chemistry, Sophia University, 7-1 Kioi-cho, Chiyoda-ku, Tokyo 102-8854, Japan (Received March 18, 2006; Accepted June 22, 2006) A series of experiments was conducted in which boron minerals were precipitated by water evaporation from solutions containing boron and potassium, sodium or lithium at 25°C, and boron isotope fractionation accompanying such mineral precipitation was investigated. In the boron-potassium ion system, K2[B4O5(OH)4]·2H2O, santite (K[B5O6(OH)4]·2H2O), KBO2·1.33H2O, KBO2·1.25H2O and sassolite (B(OH)3) were found deposited as boron minerals. Borax (Na2[B4O5(OH)4·8H2O) was found deposited in the boron-sodium ion system, and Li2B2O4·16H2O, Li2B4O7·5H2O, Li2B10O16·10H2O, LiB2O3(OH)·H2O and sassolite in the boron-lithium ion system. The boron isotopic analysis was con- 11 10 ducted for santite, K2[B4O5(OH)4]·2H2O, borax and Li2B2O4·16H2O. The separation factor, S, defined as the B/ B isotopic ratio of the precipitate divided by that of the solution, ranged from 0.991 to 1.012. Computer simulations for modeling boron mineral formations, in which polyborates were decomposed into three coor- dinated BO3 unit and four coordinated BO4 unit for the purpose of calculation of their boron isotopic reduced partition function ratios, were attempted to estimate the equilibrium constant, KB, of the boron isotope exchange between the boric – acid molecule (B(OH)3) and the monoborate anion (B(OH)4 ). -
UCLA Electronic Theses and Dissertations
UCLA UCLA Electronic Theses and Dissertations Title Use of Boron in Detergents and its Impact on Reclamation Permalink https://escholarship.org/uc/item/2rw7k2r7 Author Ghavanloughajar, Maryam Publication Date 2015 Peer reviewed|Thesis/dissertation eScholarship.org Powered by the California Digital Library University of California UNIVERSITY OF CALIFORNIA Los Angeles Use of Boron in Detergents and its Impact on Reclamation A thesis submitted in partial satisfaction of the requirements for the degree Master of Science in Civil Engineering by Maryam Ghavanloughajar 2015 ABSTRACT OF THE THESIS Use of Boron in Detergents and its Impact on Reclamation By Maryam Ghavanloughajar Master of Science in Civil Engineering University of California, Los Angeles, 2015 Professor Michael K. Stenstrom, Chair Many parts of the world are experiencing severe water drought and it affects societies both economically and environmentally. Therefore, conservation practices are essential to balance water supply and demand. Greywater or wastewaters from showers and luandries, if treated well can be a reliable source for activities such as irrigation, toilet flushing and car washing. Greywaters are not as contaminated as sewage but still may require treatment before reuse. The application of insufficiently treated water for irrigation can cause harm to plants and animals. Pollutant such as boron in greywater is of particular interest because many plants are sensitive to even low concentrations. High concentrations of boron can induce toxicity, reduce growth rate and yield in plants. Therefore, proposed greywater treatment systems need to consider the sensitivity of plant species and boron concentrations and potential removal. This thesis reviews boron chemistry, its effect on plants and currently available boron removal technologies. -
Review of the Evidence Base for the Status and Change of Soil Carbon Below 15 Cm from the Soil Surface in England and Wales
Department for Environment, Food and Rural Affairs Research project final report Project title Review of the evidence base for the status and change of soil carbon below 15 cm from the soil surface in England and Wales Sub-Project iii of Defra Project SP1106: Soil carbon: studies to explore greenhouse gas emissions and mitigation Defra project code SP1106 Contractor SKM Enviros Organisations Rothamsted Research / North Wyke Cranfield University British Geological Survey Report authors Andy Gregory ([email protected]), Andy Whitmore, Guy Kirk, Barry Rawlins, Karl Ritz, Phil Wallace. Project start date October 2010 Sub-project end date March 2011 Sub-project iii: Review of the evidence base for the status and change of soil carbon below 15 cm from the soil surface in England and Wales Executive summary The world‟s soils contain more carbon (C), predominantly in organic matter (OM), than the atmosphere and terrestrial plants combined. Our knowledge of soil C is largely restricted to the topsoil, but more than half of soil C is stored at depths lower than 15 cm in the subsoil. Subsoil C represents a little-understood component of the global C cycle, with potential implications with respect to predicted changes in climate; it is important that the level of understanding of subsoil C in England and Wales is clarified and that potential knowledge gaps are identified. The overall aim of this review was to evaluate the current status and dynamics of subsoil C in England and Wales by reviewing the best-available evidence and by sensible extrapolation. Further objectives sought to review the source and stability of subsoil C in general, to identify the key gaps in knowledge, and to seek evidence on how subsoil C may respond to imposed (soil management) or natural (climate change) changes in contributing factors in the future. -
Soil Variation
Soil Variation Have a look at some of the most common soils in Scotland’s crofting counties, as well as a couple that are only found in certain parts of the country, and how those soils are used and managed by crofters. Crofting areas in Scotland have cool and generally wet climates, which helps peat soils to develop. Ancient woodlands helped brown earth soil to form, leaching under wet and acid conditions allows podzols to form and although the woods are often gone now, the soil remains as podzols. When a soil becomes water saturated a gley soil can develop. In coastal areas crofts sometimes have soils which have developed on beach sand called Machair. The parent material influences the soil type and in a few areas the serpentinite rocks develop a rare soil called serpentine soil. 1 Peat Hi I’m Pete 2 Brown Earth Hi I’m Rusty Peat forms in very wet conditions where plant leaves, shoots As you might guess from their name brown earths are a deep and roots die and are very slowly decomposed over time. On rich brown colour, but more importantly tend to be much more average peat accumulates at about 1mm per year, is wet and fertile. They are more common on the east coast and in drier, very acid, so only those plants which are specially adapted to warmer environments. those conditions can grow. Brown earths form on rich parent material, which contains While it is not much use for farming, it is still sometimes a good balance of elements such as calcium and aluminium used as fuel (after it is dried out) and can be used to which produce pH neutral or alkaline soil. -
Design Rules for Discovering 2D Materials from 3D Crystals
Design Rules for Discovering 2D Materials from 3D Crystals by Eleanor Lyons Brightbill Collaborators: Tyler W. Farnsworth, Adam H. Woomer, Patrick C. O'Brien, Kaci L. Kuntz Senior Honors Thesis Chemistry University of North Carolina at Chapel Hill April 7th, 2016 Approved: ___________________________ Dr Scott Warren, Thesis Advisor Dr Wei You, Reader Dr. Todd Austell, Reader Abstract Two-dimensional (2D) materials are championed as potential components for novel technologies due to the extreme change in properties that often accompanies a transition from the bulk to a quantum-confined state. While the incredible properties of existing 2D materials have been investigated for numerous applications, the current library of stable 2D materials is limited to a relatively small number of material systems, and attempts to identify novel 2D materials have found only a small subset of potential 2D material precursors. Here I present a rigorous, yet simple, set of criteria to identify 3D crystals that may be exfoliated into stable 2D sheets and apply these criteria to a database of naturally occurring layered minerals. These design rules harness two fundamental properties of crystals—Mohs hardness and melting point—to enable a rapid and effective approach to identify candidates for exfoliation. It is shown that, in layered systems, Mohs hardness is a predictor of inter-layer (out-of-plane) bond strength while melting point is a measure of intra-layer (in-plane) bond strength. This concept is demonstrated by using liquid exfoliation to produce novel 2D materials from layered minerals that have a Mohs hardness less than 3, with relative success of exfoliation (such as yield and flake size) dependent on melting point. -
General Soil Map of Ireland, 1969 Survey of Some Midland Sub-Peat Mineral Soils (With Bord Na Móna), 1971 — M
SOIL SURVEY PUBLICATIONS 1962-1979 County Surveys Soils of Co. Wexford, 1964* — M. J. Gardiner and P. Ryan Soils of Co. Limerick, 1966 — T. F. Finch and P. Ryan Soils of Co. Carlow, 1967 — M. J. Conry and P. Ryan Soils of Co. Kildare, 1970 — M. J. Conry, R. F. Hammond and T. O’Shea Soils of Co. Clare, 1971 — T. F. Finch, E. Culleton and S. Diamond Soils of Co. Westmeath, 1977 — T. F. Finch and M. J. Gardiner Soils of West Cork, (part of Resource Survey) 1963 — M. J. Conry, P. Ryan and J. Lee Soils of West Donegal, (part of Resource Survey) 1969 — M. Walsh, M. Ryan and S van de Schaaf Soils of Co. Leitrim, (part of Resource Survey) 1973 — M. Walsh An Foras Talúntais Farms Grange, Co. Meath, 1962 — M. J. Gardiner Kinsealy, Co. Dublin, 1963 — M. J. Gardiner Creagh, Co. Mayo, 1963 — M. J. Gardiner Herbertstown, Co. Limerick, 1964 — T. F. Finch Drumboylan, Co. Roscommon, 1968 — G. Jaritz and J. Lee Ballintubber, Co. Roscommon, 1969 — M. Ryan and J. Lee Ballinamore, Co. Leitrim, 1969 — T. F. Finch and J. Lee Clonroche, Co. Wexford, 1970 — T. F. Finch and M. J. Gardiner Mullinahone, Co. Tipperary, 1970 — M. J. Conry Ballygagin, Co. Waterford, 1972 — T. F. Finch and M. J. Gardiner Department of Agriculture Farms Clonakilty, Co. Cork, 1964* — J. Lee and M. J. Conry Ballyhaise, Co. Cavan, 1965* — M. Ryan and J. Lee Athenry, Co. Galway, 1965* — S. Diamond, M. Ryan and M. J. Gardiner Other Farms Kells Ingram, Co. Louth, 1964* — M. J. Gardiner Multyfarnham Agricultural College, Co. -
Industrial Minerals and Rocks in the 21St Century
Industrial Minerals and Rocks in the 21st Century Milos Kuzvart Charles University, Prague NONMETALLICS: DEFINITION, CLASSIFICATION, OCCURENCE, ORIGIN, UTILIZATION The term 'industrial mineral' is not defined so strictly as the term 'ore' which is mostly a source of metal, or as that of 'fossil fuel' (coal, oil, natural gas), which is predominantly a source of energy. In both the latter cases the characteristic feature is the chemistry of the ore (besides the content of impurities, dressability, etc.) or fuel (besides the content of dirt bands, sulfur, etc.). The characteristic features of industrial minerals, however, líe in their physical properties (e.g., fibrosity of asbestos, insulatory properties of mica, the high specific gravity of barite). In this artiele raw materials of several types are considered under the term "industrial mineral s and rocks": 1. raw materials that are used in industry in variously prepared forms as minerals (e.g., talc, asbestos, diamond) or rocks (diatomite, bentonite, ochre); 2. raw material s that serve as a source of non-metallic elements (ftuorite for ftuori ne, apatite for phosphorus) or their simple compounds (e.g., borates for H3B03 or B 20 3); 3. raw materials of non-metallic habit that are source of metals, and also of their com pounds employed in other than metallurgical industries (e.g., beryl as a source of BeO, magnesite of MgO, bauxite or Al-rich laterite as a source of Alz03; all these three oxides are refractory materials); 4. building material s (rocks for aggregate, together with gravel and sand for concrete, decorative stone and roofing slate, limestone for cement and lime, brickloam). -
Soil Hydraulic Properties of Plinthosol in the Middle Yangtze River Basin, Southern China
water Article Soil Hydraulic Properties of Plinthosol in the Middle Yangtze River Basin, Southern China Yongwu Wang 1, Tieniu Wu 1,2,* , Jianwu Huang 1, Pei Tian 1,* , Hailin Zhang 1 and Tiantian Yang 3 1 Key Laboratory for Geographical Process Analysis & Simulation, Central China Normal University, Wuhan 430079, China; [email protected] (Y.W.); [email protected] (J.H.); [email protected] (H.Z.) 2 Department of Ecosystem Science and Management, The Pennsylvania State University, University Park, PA 16802, USA 3 School of Civil Engineering and Environmental Science, The University of Oklahoma, Norman, OK 73019, USA; [email protected] * Correspondence: [email protected] (T.W.); [email protected] (P.T.) Received: 16 May 2020; Accepted: 20 June 2020; Published: 23 June 2020 Abstract: Soil hydraulic properties are ecologically important in arranging vegetation types at various spatial and temporal scales. However, there is still a lack of detailed understanding of the basic parameters of plinthosol in the Middle Yangtze River basin. This paper focuses on the soil hydraulic properties of three plinthosol profiles at Yueyang (YE), Wuhan (WH), and Jiujiang (JU) and tries to reveal the origin of plinthosol and the relationship among the soil hydraulic parameters. Discriminant analysis indicated that the plinthosol in the JU profile was of aeolian origin, while that in the WH and YE profiles was of alluvial origin; soil hydraulic properties varied greatly among these profiles. The proportion of macro-aggregates (>0.25 mm, weight%) in the JU profile (88.28%) was significantly higher than that in the WH (73.63%) and YE (57.77%) profiles; the water holding capacity and saturated hydraulic conductivity of JU plinthosol was also higher than that of WH and YE plinthosol; the fact that Dr and Di of the JU profile are lower than those of the YE and WH profiles illustrates the stability of JU plinthosol is better than that of YE and WH plinthosol, which is consistent with the fractal dimension of aggregates. -
Soils of Ceylon
SOILS OF CEYLON - ANEW APPROACH TO THE IDÊNTIfICATION AND aASSIFICATlON OF THf MOST IMPORTANT SOIL'GROUPS OF CEYLON By F. R. MOORMAKN and C R. PANÄBOKKt Land use Division Hfeiation of tt>6' Department of Agriculture NATIONS CEYLON •s 1961 PRINTED AT TH8 «OVRRNlf ENT PRESS, CBÏLON, ON PAPER MANUPACTÜBBD AT THB BA9TBRN PÄPRR MItXS CORPORATION, VALAICHOHBNAI. CBÏLON, - SOILS OF CEYLON A NEW APPROACH TO THE IDENTIFICATION AND CLASSIFICATION OF THE MOST IMPORTANT SOIL GROUPS OF CEYLON By Dr. F. R. MOORMANN F.A.O. Soil Classification Consultant and Dr. C. R. PANABOKKE Head, Land Use Division, Department of Agriculture, Ceylon Scanned from original by ISRIC - World Soil Information, as ICSI) j World Data Centre for Soils. The purpose is to make a safe depository for endangered documents and to make the accrued j information available for consultation, following Fair Use J Guidelines. Every effort is taken to respect Copyright of the ] materials within the archives where the identification of the i Copyright holder is clear and, where feasible, to contact the { originators. For questions please contact [email protected] indicating the item reference number concerned. j 2 It 2251—150 (4/82) SISH CONTENTS Pag& Foreword 4 CHAPTER I Introduction CHAPTER II Great Soil Groups of Ceylon 7 1. Reddish Brown Earths & 2. Noncalcic Brown Soils 11 3. Reddish Brown Lateritie 8oils ia 4. Red-Yellow Podzolic Soils . 16 5. Red-Yellow Latosols 21 6. Immature Brown Loams 24: 7. Rendzina Soils 2ft 8. Grumusols .. .27 9. Solodized Solonetz 29> '10. Low-Humic Gley Soils 31 11. Meadow Podzolic Soils 32" 12.