330241 1 En Bookbackmatter 315..332

Total Page:16

File Type:pdf, Size:1020Kb

330241 1 En Bookbackmatter 315..332 Appendix A Ratings Tables for New Zealand Soil Properties See Tables A.1 and A.2. Table A.1 Ratings for soil chemical properties after L. C. Blakemore, P. L. Searle, and B. K. Daly 1987. Methods for chemical analysis of soils. NZ Soil Bureau Scientific Report 80. 103p. ISSN 03041735. Reproduced with permission of Manaaki Whenua – Landcare Research Rating Very high High Medium Low Very low A1: Ratings for soil pH, carbon, nitrogen, and phosphorus pH >9.0 7.1–7.5 6.0–6.5 4.5–5.2 <4.5 (1:2.5 soil: water) (extremely (slightly (slightly (strongly (extremely alkaline) alkaline) acid) acid) acid) 8.4–9.0 6.6–7.0 (near 5.3–5.9 (strongly neutral) (moderately alkaline) acid) 7.6–8.3 (moderately alkaline) Organic matter Organic carbon (%) >20 10–20 4–10 2–4<2 Total nitrogen (%) >1.0 0.6–1.0 0.3–0.6 0.1–0.3 <0.1 C/N >24 16–24 12–16 10–12 <10 Phosphorus Truog (lg/g) >50 30–50 20–30 10–20 <10 Olsen (lg/g) >50 30–50 20–30 10–20 <10 (+) −1 0.5M H2SO4 (cmol kg ) >40 20–40 10–20 5–10 <5 Inorganic (cmol(+) kg−1) >50 30–50 20–30 10–20 <10 Organic (cmol(+) kg−1) >70 50–70 20–50 10–20 <10 Total (cmol(+) kg−1) >120 80–120 40–80 20–40 <20 P retention (%) 90–100 60–90 30–60 10–30 0–10 A2: Ratings for cation exchange related properties Cation exchange CEC (cmol(+) kg−1) >40 25–40 12–25 6–12 <6 (+) −1 properties (NH4OAc, R Bases (cmol kg ) >25 15–25 7–15 3–7<3 pH7) BS (%) 80–100 60–80 40–60 20–40 <20 Ca (cmol(+) kg−1) >20 10–20 5–10 2–5<2 Mg (cmol(+) kg−1)>73–71–3 0.5–1 <0.5 K (cmol(+) kg−1) >1.2 0.8–1.2 0.5–0.8 0.3–0.5 <0.3 Na (cmol(+) kg−1) >2 0.7–2 0.3–0.7 0.1–0.3 <0.1 KCl—extract >5 2–5 0.5–2.0 0.1–0.5 <0.1 Al (cmol(+) kg−1) Exchange Acidity (pH 8.2) (cmol(+) kg−1) >60 30–60 15–30 5–15 <5 Reserve Kc >0.5 0.35–0.5 0.20–0.35 0.10–0.20 <0.10 Mgr >30 15–30 7–15 3–7<3 (continued) © The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerland AG 2021 315 A. E. Hewitt et al., The Soils of Aotearoa New Zealand, World Soils Book Series, https://doi.org/10.1007/978-3-030-64763-6 316 Appendix A: Ratings Tables for New Zealand Soil Properties Table A.1 (continued) Rating Very high High Medium Low Very low A3: Ratings for aluminium, iron, silica and sulphur contents, and soluble salts Acid oxalate— Al (%) >3.0 1.0–3.0 0.5–1.0 0.2–0.5 <0.2 extractable Fe (%) >2.0 1.0–2.0 0.5–1.0 0.2–0.5 <0.2 Si (%) >0.5 0.15–0.5 0.05–0.15 <0.05 Pyrophosphate— Al (%) >2.0 0.8–2.0 0.4–0.8 0.1–0.4 <0.1 extractable Fe (%) >1.2 0.6–1.2 0.3–0.6 0.1–0.3 <0.1 Dithionate-citrate— Al (%) >2.0 1.0–2.0 0.5–1.0 0.2–0.5 <0.2 extractable Fe (%) >4.0 2.0–4.0 1.0–2.0 0.5–1.0 <0.5 Phosphate—extractable >150 50–150 15–50 5–15 <5 sulphur or sulphate (µg S/g) Soluble salts Conductivity (millimho/cm) >2 0.8–2 0.4–0.8 0.15–0.4 <0.15 1:5 extract at 25 °C Salts (%) >0.7 0.3–0.7 0.15–0.3 0.05–0.15 <0.05 Table A.2 Ratings for soil physical properties Physical parameter Very low Low Medium High Very high Potential rooting deptha (cm) <20 20–40 40–80 80–120 >120 v. shallow shallow mod. deep deep v. deep Soil dry bulk density (g cm−3) <0.6 0.6–0.9 0.9–1.5 1.5–1.8 >1.8 Total porosity (%v/v) <35 35–45 45–60 65–75 >75 Macroporosity (%v/v) <5 5–10 10–20 20–25 >25 Penetration resistanceb (kPa) <1000 1000– 1500–2200 2200–3000 >3000 1500 Degree of packingc (kPa) <500 500–1000 1000–2200 2200–3000 >3000 loose very friable firm very friable firm Permabilityd (mm h−1) <0.4 0.4–4 4–18 18–72 >72 extremely slow moderately moderate rapid slow slow Profile readily available watera (mm) over potential rooting depth <25 25–50 50–100 100–130 >130 or 1.5 m depth Soil depthd (cm) <20 20–45 45–100 >100 very shallow moderately deep deep shallow aFrom A. D. Wilson and D. J. Giltrap 1984. Soil evaluation and classification system for orchard crop production. Soil Resources Report SR6. Soil Bureau, DSIR. 54p bAdapted from E. Griffiths 1984. Interpretation of soil morphology for assessing moisture movement and storage. NZ Soil Bureau Scientific Report 74, 20p cDetermined using Singleton Blade and 6 mm tip penetrometer after E. Griffiths 1984. Interpretation of soil morphology for assessing moisture movement and storage. NZ Soil Bureau Scientific Report 74, 20p dAdapted from S-map ratings Appendix B Correlation of Orders of New Zealand Soil Classification with the Nearest Equivalent Taxa of Soil Taxonomy and World Reference Base NZ Soil Soil Taxonomy World Reference NZ Soil Soil Taxonomy World Reference Classification Equivalent soil order (or Base Classification Equivalent soil order (or Base Soil order suborder/great group) Equivalent Soil order suborder/great group) Equivalent reference soil reference soil group group Allophanic Andisols (except Vitrands) Andosols Raw Soils Not-soil or Entisols Regosols, Soils Arenosols or Anthropic Entisols or unclassified Anthrosols or unclassified Soils Technosols Recent Soils Entisols (also Inceptisols) Fluvisols, Brown Soils Inceptisols (also Entisols) Cambisols Arenosols, Gley Soils Aquic suborders of Gleysols Leptosols, Inceptisols, Entisols, Cambisols, Oxisols, etc. Regosols, or Umbrisols Granular Ultisols Nitisols Soils Semiarid Aridisols Luvisols, Soils Cambisols, or Melanic Soils Mollisols, Vertisols Vertisols, Solonetz Calcisols, Chernozems or Ultic Soils Ultisols Planosols a Phaeozems After Hewitt (2010), Soil Survey Staff (2014) and World Reference — Organic Soils Histosols Histosols Base (2015). The correlations given here are a guide only for accurate classifications of a specific soil the soil properties and details of the Oxidic Soils Oxisols Ferralsols particular classification documents should be consulted Pallic Soils Alfisols, Inceptisols Cambisols, Hewitt AE (2010) New Zealand Soil Classification. 3rd edn. Landcare Luvisols, or Research Science Series No. 1. Lincoln, Manaaki Whenua Press 136 p Planosols Soil Survey Staff (2014) Keys to Soil Taxonomy, 12th ed. USDA Podzol Soils Spodosols Podzols Natural Resources Conservation Service, Washington, DC 362 p Pumice Soils Andisols: mainly Andosols World Reference Base (2015) http://www.fao.org/3/i3794en/I3794en. Vitrands (also Vitricryands, pdf accessed on 2 March 2020 Vitraquands) (continued) © The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerland AG 2021 317 A. E. Hewitt et al., The Soils of Aotearoa New Zealand, World Soils Book Series, https://doi.org/10.1007/978-3-030-64763-6 Index A Animals, 2, 7, 8, 10, 31, 36, 38, 55, 62, 69, 82, 83, 99, 117, 128, 159, Abrasion, 4, 61, 154, 271, 272 192, 194–196, 199, 203, 212, 219, 228, 245, 283, 290, 292, 302 Acid sulphate soils, 212 Antarctica, 2, 211, 267, 268, 270, 271, 275, 283, 284, 289, 291, 293, Active layer, 267–270, 276, 281, 282, 285, 286 298, 303 Adelaide Tarn, 125 Antarctic Treaty, 268, 284 Aeolian, 4, 61, 90, 136, 138, 164, 166, 169, 172, 203, 218, 235, 252, Anthropic, 1, 16, 41, 42, 44–47, 49, 50–55, 237, 293, 296 258 Anthrosol, 44, 52 Aerial photo, 221, 297, 300 Aokautere Ash, 151 Agriculture, 2, 9, 13, 17, 34, 69, 82, 83, 110, 117, 118, 127, 129, 158, Apedal, 12, 24, 38, 58, 61, 191 159, 194, 199, 212, 220, 231, 249, 262, 291, 294, 296, 297, 299, Apple, 1, 141, 263 301, 302, 307 Apricot, 231 A horizon, 10, 11, 16, 22, 25, 41, 98, 101, 102, 110, 149, 180, 188, Arable, 111, 245, 294, 299, 301, 307 200, 205, 216, 218, 219, 253, 294 Arapuni, 49 Ahuriri, 150, 212 Arenosol, 68, 211, 227 Aislabie, 7, 284 Argillans, 250 Alaska, 34, 271 Argillic, 67, 75, 88, 89, 92, 95, 105, 106, 148, 149, 151, 155, 157–160, Alexandra, 232, 233, 258 231, 233–237, 239–241, 243, 250, 252, 253, 257, 292, 296 Alfisol, 158, 290 Argillic horizon, 89, 95, 148, 149, 151, 158, 159, 231, 234–236, 239, Alfredton, 78 241, 252, 253 Alkalinity, 12, 236, 241, 303 Argillisation, 253, 295 Allophane, 21–27, 29–31, 33, 34, 36, 38, 57, 58, 61, 65, 68, 90–92, Argilluviation, 96 139, 141, 167–169, 172, 173, 180, 188, 191, 238, 257, 291, 294, Aridic, 241 295 Aridisol, 241, 244, 290 Allophanic, 1, 9, 14, 16, 17, 21–38, 57–59, 61, 63–65, 67, 68, 80, 92, Artefacts, 46 95, 99, 105, 137, 141, 153, 154, 157, 166, 168, 169, 174, 181, Ash, 4, 9, 21, 22, 26, 87, 89–92, 95, 136, 137, 140, 153, 166, 180, 183, 186–188, 191–193, 195, 203, 218, 223, 224, 256, 257, 289, 291, 185–187, 191, 201, 205, 253, 256, 257, 261, 263, 297 293–296, 305, 306, 309 Aspect, 2, 5, 18, 61–63, 81, 98, 194 Allophanic soil material, 21, 23–25, 29, 31, 33, 34, 36, 38, 65, 67, 95, Assimilation, 117 137, 141, 174, 191–193 Aston, 194 Alluvium, 5, 9, 10, 22, 25, 28, 29, 31, 48, 57, 60, 64, 67, 76, 105, 114, Atiamuri, 194 118–121, 123, 145, 151, 153, 159, 171, 191, 193, 199, 200, 216, Auckland, 2, 4, 5, 17, 22, 34, 54, 87, 88, 90, 91, 95, 96, 134, 136, 137, 218, 223, 227, 231, 234, 236, 238, 243, 253, 254, 293–295 249–251, 253, 254, 262, 307 Almond, 61, 171, 245 Auckland Volcanic Field, 2, 4, 5, 137 Alpha-alpha′-dipyridyl, 76 Australia, 3, 110, 125, 136, 154, 169, 195, 223, 235, 244, 258, 290, 293 Alpine, 4, 5, 27, 61, 63, 154, 158, 199, 200, 203, 212–214, 242, 244, Australian plate, 2–4, 182 246, 290 Avocado, 35, 134, 141 Alpine Fault, 2, 3, 61 Awatere Valley, 148 Aluminium toxicity, 67, 68, 93, 108, 139, 140, 173, 174, 176, 240, 260 Aluminosilicate, 21, 24, 57 Amorphous, 29, 191, 238 B Anaerobic conditions, 17, 75, 76, 79, 80, 128, 129, 146, 151, 155, 196 Backslope, 154, 169, 250, 254, 255 Andept, 34 Backswamp, 28, 76, 78, 118, 121, 216, 220, 221 Andesite, 4, 22, 28, 68, 88, 105, 138, 182, 208, 291 Bacteria, 7–9, 80, 83, 212 Andesitic, 21, 22, 26, 28, 29, 31, 34, 87, 90, 91, 106, 129, 133, 136, Banana, 141 172, 180, 182, 188, 192, 205, 256, 291 Banks, 48, 83, 105, 118, 150–152, 154, 200, 205, 209, 210, 218, 221, Andisol, 22, 34, 193, 290, 291, 293, 296 222, 227 Andosol, 35, 193, 194 Banks Peninsula, 105, 150, 151, 154 Anhyorthel, 269, 273–275 Bannockburn, 52, 242, 243 © The Editor(s) (if applicable) and The Author(s), under exclusive license to Springer Nature Switzerland AG 2021 319 A.
Recommended publications
  • Depolymerization and Mineralization – Investigating N Availability by a Novel N Tracing Model
    SOIL Discuss., doi:10.5194/soil-2016-11, 2016 Manuscript under review for journal SOIL Published: 3 March 2016 c Author(s) 2016. CC-BY 3.0 License. Depolymerization and mineralization – investigating N availability by a novel 15N tracing model Louise C. Andresen1, Anna-Karin Björsne1, Samuel Bodé2, Leif Klemedtsson1, Pascal Boeckx2 and Tobias Rütting1 5 1Department of Earth Sciences, University of Gothenburg, Gothenburg, 405 30, Sweden 2Isotope Bioscience Laboratory, ISOFYS, Ghent University, Ghent, 9000, Belgium Correspondence to: Louise C. Andresen ([email protected]) Abstract. Depolymerization of soil organic matter such as proteins and peptides into monomers (e.g. amino acids) is currently thought to be the rate limiting step for N availability in terrestrial N cycles. The mineralization of free amino acids 10 (FAA), liberated by depolymerization of peptides, is an important fraction of the total N mineralization. Accurate assessment of peptide depolymerization and FAA mineralization rates is important in order to gain a better understanding of the N cycle dynamics. Due to the short time span, soil disturbance and unnatural high FAA content during the first few hours after the labelling with the traditional 15N pool dilution experiments, analytical models might overestimate peptide depolymerization rate. In this paper, we present an extended numerical 15N tracing model Ntrace which incorporates the FAA pool and related 15 N processes in order to 1) provide a more robust and coherent estimation of production and mineralization rates of FAAs; 2) and 2) suggest an amino acid N use efficiency (NUEFAA) for soil microbes, which is a more realistic estimation of soil microbial NUE compared to the NUE estimated by analytical methods.
    [Show full text]
  • Effect of Soil Chiseling on Soil Structure and Root Growth for a Clayey Soil Under No-Tillage
    Geoderma 259–260 (2015) 149–155 Contents lists available at ScienceDirect Geoderma journal homepage: www.elsevier.com/locate/geoderma Effect of soil chiseling on soil structure and root growth for a clayey soil under no-tillage Márcio Renato Nunes a,⁎, José Eloir Denardin b, Eloy Antônio Pauletto c, Antônio Faganello b, Luiz Fernando Spinelli Pinto c a University of São Paulo, “Luiz de Queiroz” College of Agriculture, Avenida Pádua Dias, 11, CEP 13418-900 Piracicaba, São Paulo, Brazil b Embrapa Trigo, Rodovia BR 285, km. 294, P.O. Box 451, CEP 99001-970 Passo Fundo, Rio Grande do Sul, Brazil c Federal University of Pelotas, Department of Soil Science, Campus Universitário s/n, P.O. Box 354, 96010-900 Pelotas, Rio Grande do Sul, Brazil article info abstract Article history: Soil chiseling under no-tillage (NT) promotes root growth in depth. This practice, however, might affect soil ag- Received 11 November 2014 gregation. This study evaluated the chiseling effects on the aggregation of a Ferralic Nitisol (Rhodic), under NT, in Received in revised form 2 June 2015 humid subtropical climate region. The treatments carried out consisted of the time that soil was kept under NT Accepted 3 June 2015 after chiseling: continuous NT for 24 months after chiseling in September 2009; continuous NT for 18 months Available online xxxx after chiseling in March 2010; continuous NT for 12 months after chiseling in September 2010; continuous NT for 6 months after chiseling in March 2011; NT in newly chiseling soil in September 2011; continuous NT without Keywords: Soil physical attributes chiseling (control).
    [Show full text]
  • Lost Cold Antarctic Deserts Inferred from Unusual Sulfate Formation and Isotope Signatures
    ARTICLE Received 15 Oct 2014 | Accepted 20 May 2015 | Published 29 Jun 2015 DOI: 10.1038/ncomms8579 Lost cold Antarctic deserts inferred from unusual sulfate formation and isotope signatures Tao Sun1,2,w, Richard A. Socki3,w, David L. Bish4, Ralph P. Harvey5, Huiming Bao1, Paul B. Niles2, Ricardo Cavicchioli6 & Eric Tonui7 The Antarctic ice cap significantly affects global ocean circulation and climate. Continental glaciogenic sedimentary deposits provide direct physical evidence of the glacial history of the Antarctic interior, but these data are sparse. Here we investigate a new indicator of ice sheet evolution: sulfates within the glaciogenic deposits from the Lewis Cliff Ice Tongue of the central Transantarctic Mountains. The sulfates exhibit unique isotope signatures, including d34Supto þ 50% for mirabilite evaporites, D17Oupto þ 2.3% for dissolved sulfate within contemporary melt-water ponds, and extremely negative d18Oaslowas À 22.2%. The isotopic data imply that the sulfates formed under environmental conditions similar to today’s McMurdo Dry Valleys, suggesting that ice-free cold deserts may have existed between the South Pole and the Transantarctic Mountains since the Miocene during periods when the ice sheet size was smaller than today, but with an overall similar to modern global hydrological cycle. 1 Louisiana State University, Baton Rouge, Louisiana 70803, USA. 2 NASA Johnson Space Center, Houston, Texas 77058, USA. 3 ESCG, NASA Johnson Space Center, Houston, Texas 77058, USA. 4 Indiana University, Bloomington, Indianapolis 47405, USA. 5 Case Western Reserve University, Cleveland, Ohio 44106, USA. 6 University of New South Wales, Sydney, New South Wales 2052, Australia. 7 Upstream Technology, BP America, Houston, Texas 77079, USA.
    [Show full text]
  • Stabilization and Destabilization of Soil Organic Matter: Mechanisms and Controls
    13F7H GEODERLIA ELSEVIER Geoderma 74 (1996) 65-105 • Stabilization and destabilization of soil organic matter: mechanisms and controls Phillip Sollins, Peter Homann, Bruce A. Caldwell Department of Forest Science Oregon State University Corvallis, OR 97331, USA Receed 1 December 1993; revised 26 July 1995; accepted 3 April 1996 Abstract We present a conceptual model of the processes by which plant leaf and root litter is transformed to soil organic C and CO 2. Stabilization of a portion of the litter C yields material that resists further transformation; destabilization yields material that is more susceptible to microbial respiration. Stability of the organic C is viewed as resulting from three general sets of characteristics. Recalcitrance comprises, molecular-level characteristics of organic substances, including elemental composition, presence of functional groups, and molecular conformation, that influence their degradation by microbes and enzymes. Interactions refers to the inter-molecular interactions between organics and either inorganic substances or other organic substances that alter the rate of degradation of those organics or synthesis of new organics. Accessibility refers to the location of organic substances with respect to microbes and enzymes. Mechanisms by which these three characteristics change through time are reviewed along with controls on those mechanisms. This review suggests that the following changes in the study of soil organic matter dynamics would speed progress: (1) increased effort to incorporate results
    [Show full text]
  • Diagenesis and Dissolution at Sinter Island (456 Yrs Bp), Taupo Volcanic Zone: Silica Stars and the Birth of Quartz
    DIAGENESIS AND DISSOLUTION AT SINTER ISLAND (456 YRS BP), TAUPO VOLCANIC ZONE: SILICA STARS AND THE BIRTH OF QUARTZ K.A.CAMPBELL1 B.Y. LYNNE1 Scientist, Geology Programme, University of Auckland, NZ. Total No of pages (Excluding Cover Page) = 7 1University of Auckland, Geology Programme, Chemistry Building, 23 Symonds Street, Auckland, N.Z. Ph. +64-9-373-7599 Proceedings 28th NZ Geothermal Workshop 2006 DIAGENESIS AND DISSOLUTION AT SINTER ISLAND (456 YRS BP), TAUPO VOLCANIC ZONE: SILICA STARS AND THE BIRTH OF QUARTZ K.A. CAMPBELL1, B.Y. LYNNE1 1 Geology Programme, University of Auckland, Auckland, New Zealand SUMMARY – Sinter Island on Lake Ohakuri (10 m x 7 m, ~3 m above lake level) in the Orakei Korako geothermal area, Taupo Volcanic Zone, New Zealand, contains a large extinct vent, domal stromatolites and bedded sinter rich in microbial filaments. Despite its young age (456 ± 35 years BP), this ancient hot- spring deposit preserves the complete diagenetic sequence of silica phase mineralogies, confirmed by X- ray diffractometry, from opal-A to opal-CT to opal-C + quartz. Corresponding nano- to micron-scale morphologies include spheres and vitreous silica botryoids, bladed lepispheres, and merged irregular silica rods. Incipient ‘fuzzy’ quartz is represented by rows of criss-crossing rods/blades that are aligned along the c-axis, but showing the typical external habit of microcrystalline quartz. No microbial fabrics are evident in quartzose samples. The deposit also experienced spatially patchy dissolution, resulting in formation of unusual morphological features for some opal-A portions of the sinter. Three intervals of silicification (thin encrusting, thick botryoidal, cemented granular cavity-fill) occurred around filament clusters during alkali-chloride thermal discharge to create a moderately dense opaline deposit.
    [Show full text]
  • The Hidden Ecological Resource of Andic Soils in Mountain Ecosystems: Evidence from Italy
    Solid Earth, 9, 63–74, 2018 https://doi.org/10.5194/se-9-63-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. The hidden ecological resource of andic soils in mountain ecosystems: evidence from Italy Fabio Terribile1,2, Michela Iamarino1, Giuliano Langella1, Piero Manna2,3, Florindo Antonio Mileti1, Simona Vingiani1,2, and Angelo Basile2,3 1Department of Agricultural Sciences, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 2CRISP, Interdepartmental Research Centre on the Earth Critical Zone, University of Naples Federico II, Via Università 100, 80055 Portici (Naples), Italy 3Institute for Mediterranean Agricultural and Forestry Systems, National Research Council of Italy, Via Patacca 85, 80056 Ercolano (Naples), Italy Correspondence: Fabio Terribile ([email protected]) Received: 9 June 2017 – Discussion started: 9 August 2017 Revised: 1 November 2017 – Accepted: 20 November 2017 – Published: 31 January 2018 Abstract. Andic soils have unique morphological, physical, 1 Introduction and chemical properties that induce both considerable soil fertility and great vulnerability to land degradation. More- Andic soils (i.e. soils with evident andosolization process) over, they are the most striking mineral soils in terms of are known to have a unique set of morphological, physi- large organic C storage and long C residence time. This is cal, and chemical soil properties. Andosolization (Ugolini especially related to the presence of poorly crystalline clay et al., 1988; Shoji et al., 1993) is a major soil-forming pro- minerals and metal–humus complexes. Recognition of andic cess regardless of whether these soils meet or do not meet soils is then very important.
    [Show full text]
  • CORNERS of NEW ZEALAND by PRIVATE CHARTER 12 Days / 11 Nights Page | 2
    CORNERS OF NEW ZEALAND BY PRIVATE CHARTER 12 days / 11 nights Page | 2 Overview ARRIVE DEPART NIGHTS DESTINATION ACCOMMODATION ROOM TYPE Day 1 Day 4 3 Queenstown Matakauri Lodge 2x Suites Day 4 Day 6 2 Wanaka Minaret Station Alpine Lodge 2x Alpine Chalets Day 6 Day 9 3 Taupo Huka Lodge 2x Junior Lodge Suites Day 9 Day 12 3 Bay of Islands The Residences at Kauri Cliffs 1x Four Bedroom Residence Accommodation Matakauri Lodge Matakauri Lodge is an alpine lakeside retreat nestled in serenely beautiful landscapes. It is spectacularly situated on Lake Wakatipu and only seven minutes away from Queenstown. The main lodge offers accommodation in twelve luxurious guest rooms and suites, with eight outlying cottages and four suites within the lodge. Each suite features a private porch, bedroom with sitting area and open fireplace as well as walk in wardrobes and a bathroom, all nestled in native forest overlooking the lake and the mountain panorama. The lodge offers guests spacious lounges, dining and living areas, all with lake views and a range of indoor and outdoor dining options, including superb private dining. Facilities include a full service luxury spa, infinity pool, a fully equipped fitness center and an elegant meeting and business center. The Owner's Cottage features four suites in a freestanding residence, private Jacuzzi, lounge, kitchen and grand courtyard. It is ideal for families, couples or friends traveling together and special celebrations. This property includes Pre-Dinner Drinks. Check In 14:00 Check Out 11:00 Corners of New Zealand by Private Charter | 12 days / 11 nights Page | 3 Minaret Station Alpine Lodge Minaret Station Alpine Lodge welcomes guests to an authentic high country New Zealand experience.
    [Show full text]
  • World Reference Base for Soil Resources 2014 International Soil Classification System for Naming Soils and Creating Legends for Soil Maps
    ISSN 0532-0488 WORLD SOIL RESOURCES REPORTS 106 World reference base for soil resources 2014 International soil classification system for naming soils and creating legends for soil maps Update 2015 Cover photographs (left to right): Ekranic Technosol – Austria (©Erika Michéli) Reductaquic Cryosol – Russia (©Maria Gerasimova) Ferralic Nitisol – Australia (©Ben Harms) Pellic Vertisol – Bulgaria (©Erika Michéli) Albic Podzol – Czech Republic (©Erika Michéli) Hypercalcic Kastanozem – Mexico (©Carlos Cruz Gaistardo) Stagnic Luvisol – South Africa (©Márta Fuchs) Copies of FAO publications can be requested from: SALES AND MARKETING GROUP Information Division Food and Agriculture Organization of the United Nations Viale delle Terme di Caracalla 00100 Rome, Italy E-mail: [email protected] Fax: (+39) 06 57053360 Web site: http://www.fao.org WORLD SOIL World reference base RESOURCES REPORTS for soil resources 2014 106 International soil classification system for naming soils and creating legends for soil maps Update 2015 FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2015 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views or policies of FAO.
    [Show full text]
  • The Muencheberg Soil Quality Rating (SQR)
    The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Zentrum fuer Agrarlandschaftsforschung (ZALF), Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 1 Draft, Nov. 2007 The Muencheberg Soil Quality Rating (SQR) FIELD MANUAL FOR DETECTING AND ASSESSING PROPERTIES AND LIMITATIONS OF SOILS FOR CROPPING AND GRAZING Lothar Mueller, Uwe Schindler, Axel Behrendt, Frank Eulenstein & Ralf Dannowski Leibniz-Centre for Agricultural Landscape Research (ZALF) e. V., Muencheberg, Germany with contributions of Sandro L. Schlindwein, University of St. Catarina, Florianopolis, Brasil T. Graham Shepherd, Nutri-Link, Palmerston North, New Zealand Elena Smolentseva, Russian Academy of Sciences, Institute of Soil Science and Agrochemistry (ISSA), Novosibirsk, Russia Jutta Rogasik, Federal Agricultural Research Centre (FAL), Institute of Plant Nutrition and Soil Science, Braunschweig, Germany 2 TABLE OF CONTENTS PAGE 1. Objectives 4 2. Concept 5 3. Procedure and scoring tables 7 3.1. Field procedure 7 3.2. Scoring of basic indicators 10 3.2.0. What are basic indicators? 10 3.2.1. Soil substrate 12 3.2.2. Depth of A horizon or depth of humic soil 14 3.2.3. Topsoil structure 15 3.2.4. Subsoil compaction 17 3.2.5. Rooting depth and depth of biological activity 19 3.2.6.
    [Show full text]
  • Diagnostic Horizons
    Exam III Wednesday, November 7th Study Guide Posted Tomorrow Review Session in Class on Monday the 4th Soil Taxonomy and Classification Diagnostic Horizons Epipedons Subsurface Mollic Albic Umbric Kandic Ochric Histic Argillic Melanic Spodic Plaggen Anthropic Oxic 1 Surface Horizons: Mollic- thick, dark colored, high %B.S., structure Umbric – same, but lower B.S. Ochric – pale, low O.M., thin Histic – High O.M., thick, wet, dark Sub-Surface Horizons: Argillic – illuvial accum. of clay (high activity) Kandic – accum. of clay (low activity) Spodic – Illuvial O.M. accumulation (Al and/or Fe) Oxic – highly weathered, kaolinite, Fe and Al oxides Albic – light colored, elluvial, low reactivity Elluviation and Illuviation Elluviation (E horizon) Organic matter Clays A A E E Bh horizon Bt horizon Bh Bt Spodic horizon Argillic horizon 2 Soil Taxonomy Diagnostic Epipedons Diagnostic Subsurface horizons Moisture Regimes Temperature Regimes Age Texture Depth Soil Taxonomy Soil forming processes, presence or Order Absence of major diagnostic horizons 12 Similar genesis Suborder 63 Grasslands – thick, dark Great group 250 epipedons High %B.S. Sub group 1400 Family 8000 Series 19,000 Soil Orders Entisols Histosols Inceptisols Andisols Gelisols Alfisols Mollisols Ultisols Spodosols Aridisols Vertisols Oxisols 3 Soil Orders Entisol Ent- Recent Histosol Hist- Histic (organic) Inceptisol Incept- Inception Alfisol Alf- Nonsense Ultisol Ult- Ultimate Spodosol Spod- Spodos (wood ash) Mollisol Moll- Mollis (soft) Oxisol Ox- oxide Andisol And- Ando (black) Gelisol
    [Show full text]
  • A Biodiversity Study of High Temperature Mud Pool Microbial Communities: Implications of Regional/Geographical Isolation and Endemism
    A BIODIVERSITY STUDY OF HIGH TEMPERATURE MUD POOL MICROBIAL COMMUNITIES: IMPLICATIONS OF REGIONAL/GEOGRAPHICAL ISOLATION AND ENDEMISM by Benjamin R. Wheeler II A thesis submitted to the Faculty of the University of Delaware in partial fulfillment of the requirements for the degree of Master of Science in Marine Studies Winter 2006 Copyright 2006 Benjamin R. Wheeler II All Rights Reserved UMI Number: 1432290 Copyright 2006 by Wheeler, Benjamin R., II All rights reserved. UMI Microform 1432290 Copyright 2006 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, MI 48106-1346 A BIODIVERSITY STUDY OF HIGH TEMPERATURE MUD POOL MICROBIAL COMMUNITIES: IMPLICATIONS OF REGIONAL/GEOGRAPHICAL ISOLATION AND ENDEMISM by Benjamin R. Wheeler II Approved: __________________________________________________________ S. Craig Cary, Ph.D. Professor in charge of thesis on behalf of the Advisory Committee Approved: __________________________________________________________ Nancy M. Targett, Ph.D. Dean of the Graduate College of Marine Studies Approved: __________________________________________________________ Conrado M. Gempesaw II, Ph.D. Vice Provost for Academic and International Programs ii ACKNOWLEDGMENTS The love and support of my family will always be my inspiration through everything that I do in life. Thank you Mom, Dad, Jim, and Mudder for always believing in me and for your overwhelming encouragement. A special thanks to Dr. Craig Cary for the opportunity to branch out into the realm of molecular biology and conduct my research in some of the most beautiful places on Earth. For those experiences, I will be forever grateful.
    [Show full text]
  • The Taupo Eruption Sequence of AD 232±10 in Aotearoa New
    地学雑誌 Journal of Geography(Chigaku Zasshi) 130(1)117­141 2021 doi:10.5026/jgeography.130.117 The 100s: Significant Exposures of the World( No. 12) The Taupō Eruption Sequence of AD 232 ± 10 in Aotearoa New Zealand: A Retrospection * * David J. LOWE and Adrian PITTARI [Received 9 June, 2020; Accepted 13 August, 2020] Abstract The Taupō eruption, also known as eruption Y, occurred in late summer to early autumn (typically late March to early April) in AD 232 10 yr at Taupō volcano, an ‘inverse’ caldera volcano underlying Lake Taupō in the central Taupō Volcanic Zone, North Island, Aotearoa New Zealand. The complex rhyolitic eruption, the most powerful eruption globally in the last 5000 years, lasted between several days and several weeks and generated five markedly contrasting pyroclastic fall deposits( units Y1 to Y5) followed by the extremely violent emplacement of a low-aspect-ratio ignimbrite( unit Y6). The fall deposits include three phreatomagmatic units, Y1, Y3, and Y4, the latter two being the products of archetypal phreatoplinian events; and two magmatic units, Y2 and Y5, the latter being the product of an exceptionally powerful plinian (previously described as ‘ultraplinian’) event with an extreme magma discharge rate around 108 to 1010 kg s-1. The pyroclastic fall-generating eruptions were followed by the climactic emplace- ment of the entirely non-welded Taupō ignimbrite( Y6). It was generated by the catastrophic collapse of the 35 to 40-km-high plinian eruption column( Y5) that produced a very-fast-moving (600 to 900 km h-1), hot( up to 500°C) pyroclastic flow( density current) that covered about 20,000 km2 of central North Island over a near-circular area ~160 km in diameter, centred on Lake Taupō, in fewer than about ten to 15 minutes.
    [Show full text]