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Paper Title (use style: paper title)
Paper Title (use style: paper title)

... results are an indication of soil strength, usually based on ruptured soil correlations. In marine and diluvium clays, DCP results are usually inaccurate representation of the soil strength (because of shaft friction). The reason we use DCP and SPT is because it is cheap, compared to other methods l ...
Sociobiology - Universidade Estadual de Feira de Santana
Sociobiology - Universidade Estadual de Feira de Santana

... low vegetation cover on the mounds results from highly compacted and leached soils as compared to adjacent lowlands and (ii) low vegetation cover reduce ant populations and diversity because of limited foraging and nesting resources. This study was carried out in four mound fields. At each mound fie ...


... interpretation. Its purpose is to provide information for regional planning and catchment management and to identify agricultural and pasture production areas. For intensive land use at the property scale, more detailed examinations should be carried out prior to development. Observation density ave ...
Excretion factors
Excretion factors

... • In order to bring clarity in exactly what data are needed for the indicator work and for the policies they serve, Eurostat launched the DireDate project • This project provided a very good overview of the data needed, and results can be seen • However, certain gaps remain, especially related to nu ...
Impact of topsoil removal for brick-making on
Impact of topsoil removal for brick-making on

... the most common method for assessing the economic value of soil in general (as opposed to nutrients specifically in the RCA). The main advantage of the approach is that it is logical, straightforward to apply (as long as relevant data such as crop yield changes over time are available) and relativel ...
Chemistry for Geologists 1.Introduction, basic definitions. Physical
Chemistry for Geologists 1.Introduction, basic definitions. Physical

... phases at fixed conditions; Effects of temperature and pressure on enthalpy and entropy. 5. Phase equilibria in simple mineral systems; How to understand and read phase diagrams (what is liquidus, solidus, solvus or lever rule?). 6. Effects of temperature and pressure on Gibbs free energy and calcul ...
Community structure of soil inhabiting nematodes in an apple
Community structure of soil inhabiting nematodes in an apple

... . Their activities regulate the size and function of fungal bacterial populations in the soil [2, 3], plant community composition [4] and rates of carbon [5] and nitrogen [6] turnover. Nematodes are of particular interest because they are the most numerous soil mesofauna and occupy all trophic consu ...
Overview of NRCS Conservation Planning
Overview of NRCS Conservation Planning

... assistance NCS provides to landowners and operators and a basic tool for landowners to manage their land, water, and related natural resources. However, based on reviews and feedback, it appears conservation planning in many field offices is driven by farm bill program requirements, with practices b ...
Networks for Research Collaboration In the Dryland West Asia
Networks for Research Collaboration In the Dryland West Asia

... official soil P test for the regionusing a 0- to 20-cmsoil depth; about 6 mgkg-~ was consideredthe critical range belowwhich a responseto fertilizer is likely. Fertilizer P rates of 10 to 20 kg ha-~ were recommended, depending on the extent of deficiency. Althoughsimilar criteria have beendevelopedf ...
THE SULFUR CYCLE
THE SULFUR CYCLE

... pedosphere, large amounts of sulfur, originally meant to maintain in deep soil and sediments, have been released into the environment. There is an increase of oxidized sulfur (SO4) in the global cycle at the expense of the storage of reduced sulfur in the Earth’s crust. ☺ SO2 is released as an air p ...
Nature template
Nature template

... Table 1 – Location of sampling sites, number of times they were sampled, bottom water salinity, bottom water dissolved oxygen (DO) concentration (mg L-1), sediment chlorophyll a (µg cm-2), extractable NH4+ concentration (nmol cm-3), and porewater sulfide (mM). Mean values and ranges for salinity and ...
Interactions among grasses, shrubs, and
Interactions among grasses, shrubs, and

... forming a patch with high plant cover. This patch type is dispersed in a low-cover matrix formed by scattered tussocks (Soriano et al. 1994). These two patch types form a two-phase mosaic structure. A global review of plant communities in different continents support the hypothesis that this type of ...
Litter decomposition rate and soil organic matter quality in a
Litter decomposition rate and soil organic matter quality in a

... al., 2011; Schmidt et al., 2011); however, in some environments, vegetation cover is a good proxy for soil C dynamics, since it controls the input and quality of litter (De Deyn et al., 2008). In turn, vegetation depends, among other factors, on soil drainage, which also influences litter decay and ...
Potential anthropogenic mobilisation of mercury and arsenic from
Potential anthropogenic mobilisation of mercury and arsenic from

... Eroded roots of hot spring systems in Northland, New Zealand consist of mineralised rocks containing sulfide minerals. Marcasite and cinnabar are the dominant sulfides with subordinate pyrite. Deep weathering and leached soil formation has occurred in a warm temperate to subtropical climate with up ...
foundation
foundation

... These footings may be slab, stepped or sloped ones. ...
Application of bioactive peptides in agriculture English
Application of bioactive peptides in agriculture English

... plants, the proportion of free amino acids in the form of absorption is very small. Further research has revealed the peptide is absorbed faster and more than free amino acids, indicating that the biological potency of the peptide and nutritional value higher than the free amino acids. This is exact ...
Plant Water Relations: Absorption, Transport and Control
Plant Water Relations: Absorption, Transport and Control

... the capillary soil water constantly (even slowly) decreases (due to evaporation from soil surface or drainage losses) and never stabilises (Fig. 2), it turn the soil water potential decreases while the matrix potential increases. This is most evident with medium and fine texture soils (for example, ...
The scientific basis of climate-smart agriculture
The scientific basis of climate-smart agriculture

... floods) as well as slow-onset hazards (such as delayed onset of seasonal rains). CSA technologies should help ameliorate the impacts of these risks both in the short term (increase the amount of production per farm, hectare, season, etc) and in the long term (decrease the variability in production o ...
soil structure stability and distribution of carbon in water
soil structure stability and distribution of carbon in water

... of SUA Nitra) were studied. In 1999, the Department of Plant Production of SUA Nitra established long-term experiment. It included two types of soil tillage (1. conventional, 2. minimal) and three treatments of fertilization (1. without fertilization, 2. crop residues together with NPK fertilizers, ...
Meta-analysis of the effects of soil properties, site factors and
Meta-analysis of the effects of soil properties, site factors and

... preferential transport, since it indicates an early tracer arrival. The results of Koestel et al. (2011) ...
Soil
Soil

... (a) Soil water. A plant cannot extract all the water in the soil because some of it is tightly held by hydrophilic soil particles. Water bound less tightly to soil particles can be absorbed by the root. ...
Linköping University Post Print Consumptive water use to feed humanity:
Linköping University Post Print Consumptive water use to feed humanity:

... expected in response to changes in consumptive water use by both natural and anthropogenic systems. Basically, consumptive use has three faces: runoff generation influenced by land cover changes; consumptive use of water withdrawn; and evaporation from water systems (reservoirs, canals, river based ...
contact area determination of agricultural tractor wheel with soil
contact area determination of agricultural tractor wheel with soil

... dependent on vertical load but if compared with inflation pressure of 100 kPa, it is less affected by vertical load and provides lower contact area values in the same range. Inflation pressure on 290 kPa offers almost independent relation with vertical load while negligibly varies in the pre-describ ...
Weathering - Kawameeh Middle School
Weathering - Kawameeh Middle School

... • Deposition is the process of laying down eroded material in a new location. • If the speed of flowing water decreases, the water can no longer carry sediment and the sediment settles at the bottom of the water. • Floodplains form when sediment settles out of rivers that flood the areas next to ...
Consumptive water use to feed humanity – curing a blind spot
Consumptive water use to feed humanity – curing a blind spot

... expected in response to changes in consumptive water use by both natural and anthropogenic systems. Basically, consumptive use has three faces: runoff generation influenced by land cover changes; consumptive use of water withdrawn; and evaporation from water systems (reservoirs, canals, river based ...
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Soil salinity control



Soil salinity control relates to controlling the problem of soil salinity and reclaiming salinized agricultural land.The aim of soil salinity control is to prevent soil degradation by salination and reclaim already salty (saline) soils. Soil reclamation is also called soil improvement, rehabilitation, remediation, recuperation, or amelioration.The primary man-made cause of salinization is irrigation. River water or groundwater used in irrigation contains salts, which remain behind in the soil after the water has evaporated.The primary method of controlling soil salinity is to permit 10-20% of the irrigation water to leach the soil, be drained and discharged through an appropriate drainage system. The salt concentration of the drainage water is normally 5 to 10 times higher than that of the irrigation water, thus salt export matches salt import and it will not accumulate.
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