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2016 Skrypnіchenko S. V., PhD of Agricultural Sciences, Associate
2016 Skrypnіchenko S. V., PhD of Agricultural Sciences, Associate

... results of our investigations the highest level of productivity is in perennial grasses 2–3 years of use (89 and 96 t/ha of hay). Starting from 4th year of use, performance, declined to 70,5 kg/ha, while the yield of herbs 7–8 years was the lowest and amounted to 47,2 and 38,5 t/ha. Conclusion. Unde ...
Forest Soils vs. Agricultural Soils
Forest Soils vs. Agricultural Soils

... chemical properties when compared to agricultural soils. The O horizon is usually more important in forest soil, as it is a primary source of nutrients. Agricultural soils associated with rangelands and grasslands often have horizons similar to forested soils. However, if they are being cultivated, ...
Untitled - Sarton Chair
Untitled - Sarton Chair

... plagging (Blume, 2000) and later ditch and tile drainage enabled better soil tillage conditions and yields. Colonial expansion and settlement resulted in major deforestation and severe soil degradation in the Americas, Australia and Africa, in time giving rise in the 20th century to soil conservatio ...
Richmond Lake Water Quality Project: Septic Systems on Shoreline
Richmond Lake Water Quality Project: Septic Systems on Shoreline

... Richmond Lake shoreline septic systems require special consideration. That's because soil and water conditions near the shoreline may make the systems less efficient in treating waste. This in turn could cause harmful pollutants to reach the lake. The septic system's purpose is to effectively accept ...
Al NEWBURY LOCAL PLAN SITE 15: DARK LANE, TILEHURST
Al NEWBURY LOCAL PLAN SITE 15: DARK LANE, TILEHURST

... agricultural and horticultural crops can be grown and commonly includes top fruit, soft, fruit, salad crops and winter harvested vegetables. Yields are high and less variable than on land of lower quality. Grade 2 : Very Good Quality Agricultural Land Land with minor limitations which affect crop yi ...
Geomorphological survey of the area of archaeological site Bosilkovo
Geomorphological survey of the area of archaeological site Bosilkovo

... eluvial-soil formation processes. The Chalcolithic pottery was found in it. Probably the anthropogenic influence during the Chalcolithic developed in this part of the soil when it was in the beginning of its formation, e.g. transformation of eluvium into soil when the stage of humification had start ...
PRINTER`S NO. 3178 THE GENERAL ASSEMBLY OF
PRINTER`S NO. 3178 THE GENERAL ASSEMBLY OF

... Scientist in July 1974, Mr. Lipscomb assisted with field program appraisals and contributed to or managed soil survey manuscripts; and WHEREAS, Mr. Lipscomb served as State Soil Scientist from 1981 until his retirement in March 1994; and WHEREAS, Throughout his career Mr. Lipscomb worked cooperative ...
Basic Concepts and Definitons
Basic Concepts and Definitons

... parent material, and time. Soil classification is categorization of soils in groups at varying levels of generalization according to their morphological properties and/or assumed genesis in a manner important for the objectives of the classification. Many systems have been and are being used. The ma ...
Interpreting Nitrate Concentration in Tile Drainage Water
Interpreting Nitrate Concentration in Tile Drainage Water

... relationship between concentration and flow volume and the fact that identical management systems may have different water quality impacts due to differences in hydrology. Tile Spacing: Since inter-tile spacing alters the rate of water movement through the soil, it should also affect water quality. A ...
The challenges of agricultural diffuse pollution
The challenges of agricultural diffuse pollution

... of fertilizers and the mode of application, 5) rules for a. calculating fertilization rates and methods, including fractionating their application; b. use of alternating crops; and c. performing soil analysis before fertilization; this allows for calculating maximum acceptable yearly irrigation dept ...
silicate agrominerals as nutrient sources and as soil conditioners for
silicate agrominerals as nutrient sources and as soil conditioners for

... On the other hand, tropical agricultural soils are the result of a very long process of chemical weathering action. The minerals of the kaolinite group and oxides and hydroxides of iron and aluminum are the most abundant in these soils. This mineralogical composition gives low CEC and electropositiv ...
Name…………………………………………………
Name…………………………………………………

... d) Five form four students conducted a field study on rocks within the local environment of their school. (i) Formulate four objectives that could have used in their study. ...
The Water Cycle
The Water Cycle

... Living organisms also move water about. Water, either directly consumed as liquid or extracted from food, is carried within bodies. It then leaves as a gas during respiration, is excreted, or may evaporate from the skin as perspiration. Plants are the major biotic movers of water. Their roots collec ...
ISOLATION OF AN ANTIBIOTIC PRODUCER FROM SOIL
ISOLATION OF AN ANTIBIOTIC PRODUCER FROM SOIL

... You need to bring a soil sample for this class. An area around trees or bushes, or flowers. Dry, sun-baked soil is not the best sample. You need only a gram of specimen. Soil is the major reservoir of microorganisms that produce antibiotics. Considering that soil is densely packed with microorganism ...
What is Soil Organic Matter? - AgEBB
What is Soil Organic Matter? - AgEBB

... • Buffers changes in soil properties due to disturbance or variation in other environmental factors (e.g. climate). • Reduces environmental contamination and soil loss. • Possibly reduces need for external inputs and enhances internal recycling when crop residues and/or organic soil amendments are a ...
Weathering, Erosion, Deposition, and Landscapes
Weathering, Erosion, Deposition, and Landscapes

... If more snow accumulates in the winter than melts in the summer, the snow on the bottom turns to ice glacial retreat ...
Soil Invertebrates and Abiotic Factors
Soil Invertebrates and Abiotic Factors

... The Ecology of Soil Invertebrates The soil is a radically different environment for life than the ones on and above the ground; yet the essential requirements do not differ. Like organisms that live outside the soil, life in the soil requires living space, oxygen, food, and water. Without the prese ...
Manure Management Plan Writing for the Equine Owner – Part III
Manure Management Plan Writing for the Equine Owner – Part III

... • Maintain an average vegetation height across the pasture during the growing season at least 3 inches high ...
Open Education Resource Study of soil formation and physical
Open Education Resource Study of soil formation and physical

... necessary for plant growth. Also, if oxygen is present in the soil, micro-organisms will grow there which eventually are helpful for crop growth. pH of the soil should be between 6 to 8: pH of the soil should be between 6 to 8 for proper crop growth This is because, in this pH, nutrient movement wil ...
Challenges in Dryland Agriculture - A Global Perspective
Challenges in Dryland Agriculture - A Global Perspective

... from the root (Rhodes and Gerdeman, 1975). The symbiotic exchanges between VAM-fungi and the biota of soil microsites not reached by roots are taking on a new signiíicance in an agricultural research environment increasingly dominated by the imperatives of soil and water conservation (CAST, 1982). T ...
Anemone `Honorine Jobert` - Woodinville Water District
Anemone `Honorine Jobert` - Woodinville Water District

... Anemone 'Honorine Jobert' is a vigorous, fibrous-rooted, mounding, compact Japanese anemone hybrid cultivar that spreads by creeping rhizomes. Large single white flowers with yellow centers appear on long, wiry-but-graceful, branching stems over an attractive foliage mound of dark green leaves. It h ...
powdery mildew control with benomyl for greenhouse
powdery mildew control with benomyl for greenhouse

... more susceptible than Pink Round; however Pink Round was more severely affected by the root rot pathogen, Thielaviopsis basicola-only eight plants survived in the untreated checks. The remaining plants were stunted and weakened and thus had lower mildew ratings. Powdery mildew fungi tend to build up ...
OLADIPO PRESENTATION SOIL - Soil Science Society of Nigeria
OLADIPO PRESENTATION SOIL - Soil Science Society of Nigeria

... degraded or lost to water and wind erosion of topsoil, 300m hectares has been so severely degraded it cannot produce food, Arable land loss is estimated at 30 to 35 times the historical rate. Land degradation directly affects 1.5 billion people globally. In the drylands, due to drought and desertifi ...
Catalase, protease and urease activity in some types of soil
Catalase, protease and urease activity in some types of soil

... ABSTRACT: Enzymes in the soil are closely related to the physical, chemical and biological characteristics of the soil and regulate the formation of soil fertility, organic matter, nutrient mineralization and cycling in nature. Soil contains phosphatase, urease, dehydrogenase, catalase, peroxidase, ...
Development of specific bacterial detoxification enzymes as bioindicators and
Development of specific bacterial detoxification enzymes as bioindicators and

... extent of soil contamination and the requirements for remediation. As an output of this project, it is recommended that the GC-MS assay could be further developed so that when the Soil Framework Directive is introduced, and legally implemented in all member member states of the EU, a large number of ...
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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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