Soil Quality Assessment Based on a Minimum Data Set: a Case Study of a County in the Typical River Delta Wetlands
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Qingdao Port International Co., Ltd. 青島港國際股份有限公司
Hong Kong Exchanges and Clearing Limited and The Stock Exchange of Hong Kong Limited take no responsibility for the contents of this announcement, make no representation as to its accuracy or completeness, and expressly disclaim any liability whatsoever for any loss howsoever arising from or in reliance upon the whole or any part of the contents of this announcement. Qingdao Port International Co., Ltd. 青 島 港 國 際 股 份 有 限 公 司 (A joint stock company established in the People’s Republic of China with limited liability) (Stock Code: 06198) VOLUNTARY ANNOUNCEMENT UPDATE ON THE PHASE III OF OIL PIPELINE PROJECT This is a voluntary announcement made by Qingdao Port International Co., Ltd. (the “Company”, together with its subsidiaries, the “Group”). Reference is made to the voluntary announcement of the Company dated 28 December 2018, in relation to the groundbreaking ceremony for the phase III of the Dongjiakou Port-Weifang-Central and Northern Shandong oil pipeline construction project (the “Phase III of Oil Pipeline Project”). The Phase III of Oil Pipeline Project was put into trial operation on 8 January 2020. As of the date of this announcement, the Dongjiakou Port-Weifang-Central and Northern Shandong oil pipeline has extended to Dongying City in the north, opening the “Golden Channel” of crude oil industry chain from the Yellow Sea to the Bohai Bay. SUMMARY OF THE PHASE III OF OIL PIPELINE PROJECT The Phase III of Oil Pipeline Project is the key project for the transformation of old and new energy in Shandong Province, and the key construction project of the Group. -
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. -
Progressive and Regressive Soil Evolution Phases in the Anthropocene
Progressive and regressive soil evolution phases in the Anthropocene Manon Bajard, Jérôme Poulenard, Pierre Sabatier, Anne-Lise Develle, Charline Giguet- Covex, Jeremy Jacob, Christian Crouzet, Fernand David, Cécile Pignol, Fabien Arnaud Highlights • Lake sediment archives are used to reconstruct past soil evolution. • Erosion is quantified and the sediment geochemistry is compared to current soils. • We observed phases of greater erosion rates than soil formation rates. • These negative soil balance phases are defined as regressive pedogenesis phases. • During the Middle Ages, the erosion of increasingly deep horizons rejuvenated pedogenesis. Abstract Soils have a substantial role in the environment because they provide several ecosystem services such as food supply or carbon storage. Agricultural practices can modify soil properties and soil evolution processes, hence threatening these services. These modifications are poorly studied, and the resilience/adaptation times of soils to disruptions are unknown. Here, we study the evolution of pedogenetic processes and soil evolution phases (progressive or regressive) in response to human-induced erosion from a 4000-year lake sediment sequence (Lake La Thuile, French Alps). Erosion in this small lake catchment in the montane area is quantified from the terrigenous sediments that were trapped in the lake and compared to the soil formation rate. To access this quantification, soil processes evolution are deciphered from soil and sediment geochemistry comparison. Over the last 4000 years, first impacts on soils are recorded at approximately 1600 yr cal. BP, with the erosion of surface horizons exceeding 10 t·km− 2·yr− 1. Increasingly deep horizons were eroded with erosion accentuation during the Higher Middle Ages (1400–850 yr cal. -
A New Soil Quality Index (SQI) for Assessing Forest Soil Health
Soil Vital Signs: A New Soil Quality Index (SQI) for Assessing Forest Soil Health Michael C. Amacher, Katherine P. O’Neill, and Charles H. Perry May 2007 United States Forest Service Rocky Mountain Research Paper Department Research Station RMRS-RP-65WWW of Agriculture Amacher, Michael C.; O’Neil, Katherine P.; Perry, Charles H. 2007. Soil vital signs: A new Soil Quality Index (SQI) for assessing forest soil health. Res. Pap. RMRS-RP-65WWW. Fort Collins, CO: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station. 12 p. Abstract __________________________________________ The Forest Inventory and Analysis (FIA) program measures a number of chemical and physical properties of soils to address specific questions about forest soil quality or health. We developed a new index of forest soil health, the soil quality index (SQI), that integrates 19 measured physical and chemical properties of forest soils into a single number that serves as the soil’s “vital sign” of overall soil quality. Regional and soil depth differences in SQI values due to differences in soil properties were observed. The SQI is a new tool for establishing baselines and detecting forest health trends. Keywords: forest soil health, Forest Inventory and Analysis, soil indicator database, soil quality index The Authors Michael C. Amacher is a research soil scientist with the Forest and Woodland Program Area at the Forestry Sciences Laboratory in Logan, UT. He holds a B.S. and a M.S. in chemistry and a Ph.D. in soil chemistry, all from The Pennsylvania State University. He joined the Rocky Mountain Research Station in 1989. -
Sustaining the Pedosphere: Establishing a Framework for Management, Utilzation and Restoration of Soils in Cultured Systems
Sustaining the Pedosphere: Establishing A Framework for Management, Utilzation and Restoration of Soils in Cultured Systems Eugene F. Kelly Colorado State University Outline •Introduction - Its our Problems – Life in the Fastlane - Ecological Nexus of Food-Water-Energy - Defining the Pedosphere •Framework for Management, Utilization & Restoration - Pedology and Critical Zone Science - Pedology Research Establishing the Range & Variability in Soils - Models for assessing human dimensions in ecosystems •Studies of Regional Importance Systems Approach - System Models for Agricultural Research - Soil Water - The Master Variable - Water Quality, Soil Management and Conservation Strategies •Concluding Remarks and Questions Living in a Sustainable Age or Life in the Fast Lane What do we know ? • There are key drivers across the planet that are forcing us to think and live differently. • The drivers are influencing our supplies of food, energy and water. • Science has helped us identify these drivers and our challenge is to come up with solutions Change has been most rapid over the last 50 years ! • In last 50 years we doubled population • World economy saw 7x increase • Food consumption increased 3x • Water consumption increased 3x • Fuel utilization increased 4x • More change over this period then all human history combined – we are at the inflection point in human history. • Planetary scale resources going away What are the major changes that we might be able to adjust ? • Land Use Change - the world is smaller • Food footprint is larger (40% of land used for Agriculture) • Water Use – 70% for food • Running out of atmosphere – used as as disposal for fossil fuels and other contaminants The Perfect Storm Increased Demand 50% by 2030 Energy Climate Change Demand up Demand up 50% by 2030 30% by 2030 Food Water 2D View of Pedosphere Hierarchal scales involving soil solid-phase components that combine to form horizons, profiles, local and regional landscapes, and the global pedosphere. -
Soil Quality 1
START FARMINGSOIL QUALITY 1 introduction to soils Soil Quality Culman Steve ealthy soils yield healthy crops, But what is healthy soil and how do we Healthy, high-quality soil has: Hachieve it? • Good soil tilth • Sufficient depth Soil health is the foundation of productive farming practices. Fertile soil provides essential nutrients to • Sufficient, but not excessive, nutrient supply plants. Important physical characteristics of soil-like • Small population of plant pathogens and insect structures and aggregation allow water and air to pests infiltrate, roots to explore, and biota to thrive. Diverse • Good soil drainage and active biological communities help soil resist • Large population of beneficial organisms physical degradation and cycle nutrients at rates to • Low weed pressure meet plant needs. Soil health and soil quality are terms • No chemicals or toxins that may harm the crop used interchangeably to describe soils that are not • Resilience to degradation and unfavorable only fertile but also possess adequate physical and conditions biological properties to “sustain productivity, maintain —from Soil Health Training Manual environmental quality and promote plant and animal health” (Doron 1994). According to the (USDA) Natural Resource Remember, soil fertility is only one component Conservation Service, “Soil quality is how well soil does of soil quality. Fertile soils are able to provide the what we want it to do.” In order to grow our crops, we nutrients required for plant growth. These are the want the soil to hold water and nutrients like a sponge chemical components of soil. Some plants need certain where they are readily available for plant roots to take nutrients in large amounts, like nitrogen, phosphorus, them up, suppress pests and weeds that may attack and potassium, which are called macronutrients. -
A Harmonious Satellite-Unmanned Aerial Vehicle-Ground Measurement Inversion Method for Monitoring Salinity in Coastal Saline Soil
remote sensing Article A Harmonious Satellite-Unmanned Aerial Vehicle-Ground Measurement Inversion Method for Monitoring Salinity in Coastal Saline Soil Suming Zhang and Gengxing Zhao * National Engineering Laboratory for Efficient Utilization of Soil and Fertilizer Resources, College of Resources and Environment, Shandong Agricultural University, Taian 271018, China * Correspondence: [email protected]; Tel.: +86-133-4528-3157 Received: 22 May 2019; Accepted: 12 July 2019; Published: 18 July 2019 Abstract: Soil salinization adversely impacts crop growth and production, especially in coastal areas which experience serious soil salinization. Therefore, rapid and accurate monitoring of the salinity and distribution of coastal saline soil is crucial. Representative areas of the Yellow River Delta (YRD)—the Hekou District (the core test area with 140 sampling points) and the Kenli District (the verification area with 69 sampling points)—were investigated. Ground measurement data, unmanned aerial vehicle (UAV) multispectral imagery and Sentinel-2A multispectral imagery were used as the data sources and a satellite-UAV-ground integrated inversion of the coastal soil salinity was performed. Correlation analyses and multiple regression methods were used to construct an accurate model. Then, a UAV-based inversion model was applied to the satellite imagery with reflectance normalization. Finally, the spatial and temporal universality of the UAV-based inversion model was verified and the soil salinity inversion results were obtained. The results showed that the green, red, red-edge and near-infrared bands were significantly correlated with soil salinity and the spectral parameters significantly improved this correlation; hence, the model is more effective upon combining spectral parameters with sensitive bands, with modeling precision and verification precision of the best model being 0.743 and 0.809, respectively. -
Willamette Valley Soil Quality Card Guide to Accompany the Willamette Valley Soil Quality Card, EM 8711
Willamette Valley Soil Quality Card Guide To accompany the Willamette Valley Soil Quality Card, EM 8711 EM 8710-E Reprinted February 2009 Contents Introduction ......................................................................................................................................3 Suggested assessment calendar ........................................................................................................4 Soil-quality indicators 1. Does the soil have good structure and tilth? ..........................................................................5 2. Is the soil free of compacted layers? ......................................................................................7 3. Is the soil worked easily? .......................................................................................................9 4. Is the soil full of living organisms? ......................................................................................11 5. Are earthworms abundant in the soil? .................................................................................13 6. Is plant residue present and decomposing? ..........................................................................15 7. Do crops/weeds appear healthy and vigorous? ....................................................................17 8. Do plant roots grow well? ....................................................................................................19 9. Does water infiltrate quickly? ..............................................................................................21 -
Inherent Factors Affecting Soil Organic Matter
Soil organic matter (SOM) is the organic component of soil, consisting of three primary parts including small (fresh) plant residues and small living soil organisms, decomposing (active) organic matter, and stable organic matter (humus). Soil organic matter serves as a reservoir of nutrients for crops, provides soil aggregation, increases nutrient exchange, retains moisture, reduces compaction, reduces surface crusting, and increases water infiltration into soil. Components vary in proportion and have many intermediate stages (Figure 1). Plant residues on the soil surface such as leaves, manure, or crop residue are not considered SOM and are usually removed from soil samples by sieving through a 2 mm wire mesh before analysis. Soil organic matter content can be estimated in the field and tested in a lab to provide estimates for Nitrogen, Phosphorus and Sulfur mineralized available for crop production and adjust fertilizer recommendations. Soil organic matter impacts the rate of surface applied herbicides along with soil pH necessary to effectively control weeds. Soil organic matter impacts the potential for herbicide carryover for future crops, and amount of lime necessary to raise pH. Figure 1. Major soil organic matter components (Source: The Soil Food Web, USDA-NRCS). Inherent Factors Affecting Soil Organic Matter Inherent factors affecting soil organic matter such warm and humid and slower in cool, dry climates. as climate and soil texture cannot be changed. Organic matter also decomposes faster when soil is Climatic conditions, such as rainfall, temperature, well aerated (higher oxygen levels) and much moisture, and soil aeration (oxygen levels) affect slower on saturated wet soils (refer to soil the rate of organic matter decomposition. -
Scopes and Limits of Soil Evaluation in Urban Planning Procedures Markus TUSCH, Clemens GEITNER and Jörn DITTFURTH Mag
reviewed paper A Thematic Soil Plan for the City of Munich – Scopes and Limits of Soil Evaluation in Urban Planning Procedures Markus TUSCH, Clemens GEITNER and Jörn DITTFURTH Mag. Markus Tusch, University of Innsbruck, Inst. of Geography, Innrain 52, A-6020 Innsbruck, [email protected] 1 SOIL AS COMPONENT OF THE URBAN ECOSYSTEM Soil as the top layer of the earth’s crust, formed by mineral particles, organic matter, water, air and living organisms performs a variety of ecological, social and economic functions vital for human life. Nevertheless the ecological value and significance of intact soils is often grossly underrated compared to the economic value of land. Especially in densely populated areas soils and their manifold functions are impaired and endangered by sealing, compaction, contamination or outright removal. In Germany the conservation of soil is therefore regulated by the German Federal Soil Protection Act (BBodSchG 1998). However, until recently soil played but a minor role in urban planning procedures mainly due to a lack of interpreted, planning- oriented information concerning urban soils and their natural functions. Information about "soil" is usually limited to the economic value, i.e. real estate value or land price, to known or assumed contaminations, to the degree of surface sealing and to the mechanical and geohydrological suitability as building ground. Comparatively little is known about the potential of local soils to develop biotopes for animals and plants, about soil performances in carbon, nutrient and water cycles – e.g. the capacity to infiltrate rain water – or soils’ capacity to filter, buffer and transform potentially harmful substances. -
Soils in Landscaped Public Areas - Wolfgang Burghardt
AGRICULTURAL SCIENCES – Vol. II - Soils in Landscaped Public Areas - Wolfgang Burghardt SOILS IN LANDSCAPED PUBLIC AREAS Wolfgang Burghardt Institute of Ecology, University of Essen, Germany Keywords: soil, park, playground, burial ground, soil pollution, soil compaction, pollution, aeration Contents 1. Introduction 2. Parks 3. Playgrounds 4. Burial Grounds Glossary Bibliography Summary Demands of public use determine the quality of urban ground and soils. On the other hand city history, location and availability of the ground have greater influence on the use than do the soil characteristics. In addition the use of the ground and the urban environment can effect the soil in an extreme way. This mutual relationship is pronounced for soils of parks, cemeteries and playgrounds. To a minor extent, very old remnant areas survive in many cities. They can have well developed soil morphology, not touched by agriculture, of low maintenance input and are in many respects in a natural state, but which are under the impact of the environment of urban atmosphere. Often they are strongly acid and can be a source of groundwater pollution. Most areas are exposed to landscaping by tipping and excavation. The reasons for this are numerous. New substrates are the body of soil formation. These soils are young and not much developed or stratified into horizons. Accumulation of humus will be visible, indicating that the soils are already sinks for carbon dioxide. An adverse characteristic of soils tippedUNESCO in the last 30 to 40 years –is strong EOLSS compaction, which is not found to the same extent in rural areas. Compaction can be dominant. -
The Comprehensive Evaluation on Resource Environmental Bearing Capacity of Central Cities in the Yellow River Delta-A Case Study on Dongying City
JouJournalr noaf lGr ofou Grnoudwnadtwera Stecri eSncceien acend a Endn gEineengineeringr ing V o l.V5o l .5N o .N4 o .4D ec D. ec2017. 2017 The comprehensive evaluation on resource environmental bearing capacity of central cities in the Yellow River Delta-A case study on Dongying City WANG Kui-feng1,2,3*, XU Meng1, CHEN Xiao-man4 1 Shandong Institute and Laboratory of Geological Sciences, Key Laboratory of Geological Process and Resource Utilization of Metallic Minerals in Shandong, Key Laboratory of Gold Mineralization Process and Resource Utilization Subordinate to the Ministry of Land and Resource, Jinan 250013, China. 2 Key Laboratory of Assessing Resource Environmental bearing capacity, Ministry of Land and Resources (Chinese Academy of Land and Resource Economics, China University of Geosciences in Beijing), Beijing 101149, China. 3 School of Civil Engineering, Shandong University, Jinan 250061, China. 4 Guangdong Research Center for Geoanalysis, Guangzhou, Guangdong Province 510080, China. Abstract: Dongying City, which is the most important central city in the Yellow River Delta, is located in the estuary of the Yellow River. With a short land formation time, ecological environment is very weak in this area. To realize the sustainable economic development of the Yellow River Delta, resource environment and resource environmental bearing capacity (REBC) must be improved. This study builds assessment system of regional REBC through resource and economic characteristics in Yellow River Delta and uses principal component analysis (PCA) method to evaluate REBC of five counties and districts in Dongying City in 2011-2015 on the dimensions of time and space. Results show that, on the time dimension, Guangrao County is ranked first, Dongying district second for four years and Hekou and Kenli districts with lower ranks in 2012-2015, indicating that more attention needs to be paid to REBC of Hekou and Dongying districts and these two districts should be included into key monitoring areas.