This document provides a summary of the different types of soils found in India. It discusses 8 major groups of Indian soils: alluvial soils, black soils, red soils, laterite and lateritic soils, forest and mountain soils, arid and desert soils, saline and alkaline soils, and peaty and marshy soils. For each group, it describes their characteristics, chemical properties, distribution across India, and common crops grown in those soil types. The summary focuses on providing a high-level overview of the key soil groups and the factors involved in their formation and classification.
Soils in India are formed by the weathering of rocks and are influenced by climate, vegetation, relief and parent material. The eight major soil types according to ICAR are alluvial, black, red, laterite, desert, mountain, saline/alkaline and peaty/marshy soils. Alluvial soils cover a large area and are highly fertile, supporting agriculture. Soil erosion due to deforestation, overgrazing and other factors needs to be controlled through conservation measures like contour farming and afforestation.
This document provides information about different types of soils found in India. It discusses alluvial soil, black soil, red soil, mountain soil, desert soil, saline and alkaline soils, peaty and marshy soils, residual soils, marine soils, glacial soils, and wind-blown soils. For each soil type, it describes where they are found, how they are formed, their composition and properties. The document aims to educate the reader about the various soils across India and their characteristics.
The document summarizes the different types of soils found in India according to the Indian Council of Agricultural Research (ICAR). It discusses 8 major types of soils - alluvial soil, black cotton soil, red and yellow soil, laterite soil, mountain or forest soil, arid or desert soil, saline and alkaline soil, and peaty and marshy soil. Each type is described in terms of its composition, location within India, agricultural usage, and distinguishing characteristics. Key crops grown in each soil type are also mentioned.
The document provides information on the classification of soils in India according to the Indian Council of Agricultural Research (ICAR). It discusses the eight main types of soils in India - alluvial soil, black cotton soil, red and yellow soil, laterite soil, mountainous or forest soil, arid or desert soil, saline and alkaline soil, and peaty and marshy soil. For each soil type, it provides details on their composition, location in India, characteristics, and common crops cultivated. It also discusses soil profile, soil erosion, conservation methods, and provides sample questions regarding Indian soil types that may be asked in UPSC civil services examinations.
Six main types of soil are found in India: alluvial, black, red, laterite, mountain, and desert soils. Alluvial soils are most common, found along river basins and coastal plains, and are very fertile. Black soils develop in the Deccan lava tract and are rich in nutrients but lack phosphorus and nitrogen. Red soils are found in the south and east and give crops good yields with irrigation. Laterite soils form in wet, leached conditions in southern areas. Mountain soils vary by altitude in the Himalayas. Desert soils in Rajasthan are sandy, salty, and deficient in organic matter. The shear strength of soil is important for foundation, slope, and earth retaining
The document describes the main soil groups found in India: alluvial soils, black soils, red soils, laterites and lateritic soils, and other minor groups. It provides details on the origin, characteristics, distribution, common crops, problems, and management of each soil group. Alluvial soils are formed by river deposition and come in new and old varieties. Black soils are high in clay and known for cotton and cereal production. Red soils are shallow to deep and suitable for cereals, millets, and plantation crops. Laterites are formed under tropical conditions and contain iron/aluminum oxides.
The document discusses the distribution and causes of different types of problematic soils in India, including acidic soils which cover 49 million hectares, or 9.3% of the country's total geographical area. It outlines the main factors that can lead to the formation of acidic, saline, sodic, saline-sodic, calcareous, and acid sulfate soils. Problematic soils pose challenges for agricultural land use due to their composition and environmental conditions.
This document provides a summary of the different types of soils found in India. It discusses 8 major groups of Indian soils: alluvial soils, black soils, red soils, laterite and lateritic soils, forest and mountain soils, arid and desert soils, saline and alkaline soils, and peaty and marshy soils. For each group, it describes their characteristics, chemical properties, distribution across India, and common crops grown in those soil types. The summary focuses on providing a high-level overview of the key soil groups and the factors involved in their formation and classification.
Soils in India are formed by the weathering of rocks and are influenced by climate, vegetation, relief and parent material. The eight major soil types according to ICAR are alluvial, black, red, laterite, desert, mountain, saline/alkaline and peaty/marshy soils. Alluvial soils cover a large area and are highly fertile, supporting agriculture. Soil erosion due to deforestation, overgrazing and other factors needs to be controlled through conservation measures like contour farming and afforestation.
This document provides information about different types of soils found in India. It discusses alluvial soil, black soil, red soil, mountain soil, desert soil, saline and alkaline soils, peaty and marshy soils, residual soils, marine soils, glacial soils, and wind-blown soils. For each soil type, it describes where they are found, how they are formed, their composition and properties. The document aims to educate the reader about the various soils across India and their characteristics.
The document summarizes the different types of soils found in India according to the Indian Council of Agricultural Research (ICAR). It discusses 8 major types of soils - alluvial soil, black cotton soil, red and yellow soil, laterite soil, mountain or forest soil, arid or desert soil, saline and alkaline soil, and peaty and marshy soil. Each type is described in terms of its composition, location within India, agricultural usage, and distinguishing characteristics. Key crops grown in each soil type are also mentioned.
The document provides information on the classification of soils in India according to the Indian Council of Agricultural Research (ICAR). It discusses the eight main types of soils in India - alluvial soil, black cotton soil, red and yellow soil, laterite soil, mountainous or forest soil, arid or desert soil, saline and alkaline soil, and peaty and marshy soil. For each soil type, it provides details on their composition, location in India, characteristics, and common crops cultivated. It also discusses soil profile, soil erosion, conservation methods, and provides sample questions regarding Indian soil types that may be asked in UPSC civil services examinations.
Six main types of soil are found in India: alluvial, black, red, laterite, mountain, and desert soils. Alluvial soils are most common, found along river basins and coastal plains, and are very fertile. Black soils develop in the Deccan lava tract and are rich in nutrients but lack phosphorus and nitrogen. Red soils are found in the south and east and give crops good yields with irrigation. Laterite soils form in wet, leached conditions in southern areas. Mountain soils vary by altitude in the Himalayas. Desert soils in Rajasthan are sandy, salty, and deficient in organic matter. The shear strength of soil is important for foundation, slope, and earth retaining
The document describes the main soil groups found in India: alluvial soils, black soils, red soils, laterites and lateritic soils, and other minor groups. It provides details on the origin, characteristics, distribution, common crops, problems, and management of each soil group. Alluvial soils are formed by river deposition and come in new and old varieties. Black soils are high in clay and known for cotton and cereal production. Red soils are shallow to deep and suitable for cereals, millets, and plantation crops. Laterites are formed under tropical conditions and contain iron/aluminum oxides.
The document discusses the distribution and causes of different types of problematic soils in India, including acidic soils which cover 49 million hectares, or 9.3% of the country's total geographical area. It outlines the main factors that can lead to the formation of acidic, saline, sodic, saline-sodic, calcareous, and acid sulfate soils. Problematic soils pose challenges for agricultural land use due to their composition and environmental conditions.
This document provides information about soil, including its definition, components, formation processes, types, properties, classification, surveys, and relationship with plants. It begins by defining soil from traditional, geologic, engineering, and agronomic perspectives. The main components of soil are described as being decomposition, translocation, leaching, and weathering. The document then discusses the major soil types found in India and their characteristics. It also outlines some key physical and chemical properties of soil and how soil surveys are conducted. In the end, it briefly explains the important relationship between soil and plants.
Indian soils are generally divided into four broad types. These soil types are: 1) alluvial soils; 2) regular soils; 3) red soils and 4) laterite soils.
The document discusses different types of soil found in India. It begins by thanking those who helped with the soil project. It then provides information on soil formation and describes the major soil types in India - alluvial, black, red and yellow, laterite, forest/mountain, and arid soils. For each soil type, it discusses characteristics, location, and crops grown. In total, six major soil types are described that cover different percentages of India's total land area. The document concludes with information on soil erosion and conservation methods.
This document summarizes the key soil types found in India, including alluvial soils deposited by rivers in northern plains; black soils high in clay and good for cotton/sugarcane; red soils weathered from crystalline rocks; lateritic soils leached of nutrients by heavy rainfall; forest soils high in organic matter; mountain soils shallow and rocky; desert soils sandy and alkaline but fertile with irrigation; saline/alkaline soils with high salt content; and peaty/marshy soils submerged and acidic. Each soil type is described in terms of composition, location, agricultural suitability, and distinguishing characteristics.
Soil has evolved over millions of years and is an important natural resource.
Soils in India can be classified as - Alluvial, Black, Red and Laterite soils. Their distribution, composition, characteristics such as color, texture, minerals, crops grown and it's conservation have been described.
India's soils are classified based on their formation process and location. The major soil types are black soil, red soil, laterite soil, and alluvial soil. Black soil covers around 16% of India and forms from weathered volcanic basalt rock. It is generally fertile but deficient in nutrients. Alluvial soil covers around 40% of India and forms from silt deposited by river flooding. It is found in river basins and coastal areas.
This document discusses different types of problematic soils including acidic, saline, and alkali soils. It provides details on the characteristics and causes of each soil type as well as management practices. Acidic soils have a pH below 7 and are common in India. Saline soils contain excess salts and are found in certain states. Alkali soils have a high pH and hard layers. The document also covers physical properties of problematic soils such as soil crusting, water logging, erosion, and swelling.
A Slide Of an Environment or Discoverable by Shivam and that i want public download my PowerPoint self made and i uploaded to SlideShare Slide Name: Soil Types Found In India
Thank You
Shivam Palta
the presentation is about, what is soil and what it the components of soil? And major types of soil in south Asia is found. specially in Bangladesh with necessary figure. _Parves Khan
The document discusses different classifications of soils in India based on various factors. Soils are classified based on their texture, color, location, and genesis. The major soil types include alluvial, black, red and yellow, laterite, arid, saline, peaty, and forest soils. Alluvial soils cover 40% of India and are found in river valleys and plains. They are classified further as Khadar and Bhangar soils based on their location and age of deposition.
Soil is formed through weathering and erosion of rocks over long periods of time. The main types of soil in India are black soil, red soil, alluvial soil, and laterite soil. Black soil forms from lava rock in areas like Maharashtra and is suitable for cotton. Alluvial soil covers nearly half of India and forms from silt deposited by rivers, making it fertile for crops.
The document summarizes the major soil types found in India. It begins by defining soil and its important functions. It then discusses the key factors that affect soil formation. The major soil types described include alluvial soil, black soil, red soil, laterite soil, desert soil, and mountain soil. For each soil type, the document provides details on formation, composition, geographic distribution within India, and common crops grown. The alluvial soil type is further divided into khadar and bhangar soils based on age and properties. Overall, the document concisely outlines the different soil categories in India and their distinguishing characteristics in 3 paragraphs or less.
This document classifies and describes the major soil types in India. It identifies 10 major soil types: alluvial soil, red soil, black or regur soil, arid/desert soil, laterite soil, saline soil, peaty/marshy soil, forest soil, sub-mountain soil, and snowfields. Alluvial soil covers around 43% of India's land area and is highly fertile, found in river valleys and deltas. Red soil is porous and deficient in nutrients, seen in low rainfall areas. Black soil has high water retention and is best for cotton cultivation, covering much of the Deccan.
Resource and Development nilay kapasia.pptxJAYAPATEL52
The document discusses different types of soils found in India. It describes alluvial soil, which is very fertile and found in northern plains, deposited by rivers like the Indus, Ganga and Brahmaputra. It is rich in nutrients. Black soil covers parts of central India and is ideal for cotton. Red or yellow soils are found in southern and eastern parts of the Deccan plateau. Laterite soil, rich in iron but deficient in nutrients, is found in southern states. Arid soil in parts of Rajasthan and Gujarat is saline with low humus. Forest soil in hilly and forest regions is acidic with low humus.
Introduction:
Folding, a fundamental process in structural geology, embodies the dynamic interaction between tectonic forces and the Earth's crust. Understanding the mechanics behind folding is essential for deciphering the deformation history of rock layers and unraveling the complexities of geological structures. This essay explores the mechanics of folding in structural geology, shedding light on the processes that shape the Earth's crust and drive geological evolution.
Fundamental Principles of Folding:
Folding occurs when compressional or extensional forces act upon rock layers, causing them to bend and deform. The mechanical behavior of rocks under stress is governed by principles of elasticity, plasticity, and rheology. Initially, rocks deform elastically, exhibiting reversible strain. However, as stress accumulates, rocks may undergo plastic deformation, resulting in irreversible changes in shape and structure. The rheological properties of rocks, such as their composition, temperature, and pressure conditions, influence their response to deformation and the style of folding observed.
Types of Folds:
Folds manifest in a variety of forms, each reflecting the interplay between tectonic forces and rock properties. Anticlines and synclines represent convex-upward and concave-upward folds, respectively, formed by compressional stresses. Overturned and recumbent folds involve significant tilting of the axial plane, indicating intense deformation. Monoclines and chevron folds exhibit more complex geometries, often associated with localized faulting or folding over basement structures. The diversity of fold types underscores the heterogeneous nature of tectonic processes and the intricate mechanics governing rock deformation.
Factors Influencing Folding:
Several factors influence the mechanics of folding, including the magnitude and direction of tectonic forces, the mechanical properties of rocks, and the presence of pre-existing structures. Convergent plate boundaries, where crustal plates collide, are primary sites of folding and mountain building. Divergent boundaries, characterized by crustal extension, may produce rift-related folding and basin formation. Additionally, the orientation of bedding planes, foliation, and fractures within rock layers can influence the style and orientation of folds.
Deformation Mechanisms:
The mechanisms driving folding include flexural slip, layer-parallel shortening, and buckling. Flexural slip occurs when layers of differing competence within a rock unit slide past each other, leading to the development of hinges and limbs in folds. Layer-parallel shortening involves the contraction of individual layers parallel to their bedding planes, resulting in the development of tight, closely spaced folds. Buckling occurs when compressive forces exceed the elastic limit of rocks, causing them to buckle and fold into characteristic shapes.
Conclusion:
The mechanics of folding in structural geology represent.
India has various types of soil formed by weathering of rocks under different climates and deposition by denudation agents. The six main types are alluvial, black, red, laterite, desert, and mountainous soils. Alluvial soil covers over 7.7 million square km in areas like Uttar Pradesh and covers the most extensive areas. Black soil is best for cotton and found in states like Maharashtra. Red soil covers over 5.18 lakh km2 across central and southern India. Soil erosion due to deforestation, overgrazing, and unscientific farming methods affects soil fertility and agricultural productivity. Conservation methods like terracing, afforestation, check dams, and planned grazing help
Indian soils come in 6 main types - alluvial, laterite, red, black, mountain, and desert soils. Alluvial soils are fertile soils deposited by river sediments. Laterite soils are found in southern India and are rich in iron oxides but less fertile. Red soils develop in low rainfall areas on granite and are moderately fertile. Black soils are very fertile but sticky clay soils found in central India. Mountain soils are humus-rich but low in nutrients. Desert soils are sandy, drain well but lack nutrients and blow away easily. The type of soil depends on climate, vegetation and underlying rock in each region and influences what crops can be grown.
The document discusses laterite soils found in India. Laterite soils are formed in hot, wet, tropical areas through weathering of rocks. They are shallow, acidic soils that are low in fertility. However, they are well suited to growing crops like tea, coffee, and rubber when provided with manure and irrigation. Laterite soils are widely distributed across India, particularly in the southern states of Kerala, Karnataka, Andhra Pradesh, and Tamil Nadu. They have high clay and iron oxide content but are deficient in nutrients like nitrogen.
Soils of India/ Karnataka State New syllabus/ Social Science/ Geography/ Chap...Jaidas Puthan Veetil
Soil is formed by weathering of rocks under different climates and deposited by denudation agents. The main types of soil in India are alluvial soil found in river plains, black soil suited for cotton in central India, red soil covering much of the Deccan plateau, laterite soil in high rainfall areas, desert soil in arid northwest India, and mountain soil rich in nutrients. Soil erosion due to factors like deforestation, overgrazing, and unscientific farming methods needs to be prevented through conservation methods like contour ploughing, bunds, terracing, afforestation, and controlled grazing/irrigation.
19212AGC101 Prakash Kumar Report on Organic Cultivation Of Kodo Millet PRAKASHKHURANA
Organic cultivation of Kodo millet involves growing the crop without synthetic pesticides or fertilizers. Crop rotation, companion planting, and organic fertilizers are used to control pests and enrich the soil. Kodo millet is a drought-resistant crop well-suited to dry, poor soils. It provides income for farmers and helps combat malnutrition through its nutritional value. The document discusses the preparation, planting, and care of organic Kodo millet crops.
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Similar to 19212AGC101, PRAKASH KUMAR SOILS OF INDIA.pptx
This document provides information about soil, including its definition, components, formation processes, types, properties, classification, surveys, and relationship with plants. It begins by defining soil from traditional, geologic, engineering, and agronomic perspectives. The main components of soil are described as being decomposition, translocation, leaching, and weathering. The document then discusses the major soil types found in India and their characteristics. It also outlines some key physical and chemical properties of soil and how soil surveys are conducted. In the end, it briefly explains the important relationship between soil and plants.
Indian soils are generally divided into four broad types. These soil types are: 1) alluvial soils; 2) regular soils; 3) red soils and 4) laterite soils.
The document discusses different types of soil found in India. It begins by thanking those who helped with the soil project. It then provides information on soil formation and describes the major soil types in India - alluvial, black, red and yellow, laterite, forest/mountain, and arid soils. For each soil type, it discusses characteristics, location, and crops grown. In total, six major soil types are described that cover different percentages of India's total land area. The document concludes with information on soil erosion and conservation methods.
This document summarizes the key soil types found in India, including alluvial soils deposited by rivers in northern plains; black soils high in clay and good for cotton/sugarcane; red soils weathered from crystalline rocks; lateritic soils leached of nutrients by heavy rainfall; forest soils high in organic matter; mountain soils shallow and rocky; desert soils sandy and alkaline but fertile with irrigation; saline/alkaline soils with high salt content; and peaty/marshy soils submerged and acidic. Each soil type is described in terms of composition, location, agricultural suitability, and distinguishing characteristics.
Soil has evolved over millions of years and is an important natural resource.
Soils in India can be classified as - Alluvial, Black, Red and Laterite soils. Their distribution, composition, characteristics such as color, texture, minerals, crops grown and it's conservation have been described.
India's soils are classified based on their formation process and location. The major soil types are black soil, red soil, laterite soil, and alluvial soil. Black soil covers around 16% of India and forms from weathered volcanic basalt rock. It is generally fertile but deficient in nutrients. Alluvial soil covers around 40% of India and forms from silt deposited by river flooding. It is found in river basins and coastal areas.
This document discusses different types of problematic soils including acidic, saline, and alkali soils. It provides details on the characteristics and causes of each soil type as well as management practices. Acidic soils have a pH below 7 and are common in India. Saline soils contain excess salts and are found in certain states. Alkali soils have a high pH and hard layers. The document also covers physical properties of problematic soils such as soil crusting, water logging, erosion, and swelling.
A Slide Of an Environment or Discoverable by Shivam and that i want public download my PowerPoint self made and i uploaded to SlideShare Slide Name: Soil Types Found In India
Thank You
Shivam Palta
the presentation is about, what is soil and what it the components of soil? And major types of soil in south Asia is found. specially in Bangladesh with necessary figure. _Parves Khan
The document discusses different classifications of soils in India based on various factors. Soils are classified based on their texture, color, location, and genesis. The major soil types include alluvial, black, red and yellow, laterite, arid, saline, peaty, and forest soils. Alluvial soils cover 40% of India and are found in river valleys and plains. They are classified further as Khadar and Bhangar soils based on their location and age of deposition.
Soil is formed through weathering and erosion of rocks over long periods of time. The main types of soil in India are black soil, red soil, alluvial soil, and laterite soil. Black soil forms from lava rock in areas like Maharashtra and is suitable for cotton. Alluvial soil covers nearly half of India and forms from silt deposited by rivers, making it fertile for crops.
The document summarizes the major soil types found in India. It begins by defining soil and its important functions. It then discusses the key factors that affect soil formation. The major soil types described include alluvial soil, black soil, red soil, laterite soil, desert soil, and mountain soil. For each soil type, the document provides details on formation, composition, geographic distribution within India, and common crops grown. The alluvial soil type is further divided into khadar and bhangar soils based on age and properties. Overall, the document concisely outlines the different soil categories in India and their distinguishing characteristics in 3 paragraphs or less.
This document classifies and describes the major soil types in India. It identifies 10 major soil types: alluvial soil, red soil, black or regur soil, arid/desert soil, laterite soil, saline soil, peaty/marshy soil, forest soil, sub-mountain soil, and snowfields. Alluvial soil covers around 43% of India's land area and is highly fertile, found in river valleys and deltas. Red soil is porous and deficient in nutrients, seen in low rainfall areas. Black soil has high water retention and is best for cotton cultivation, covering much of the Deccan.
Resource and Development nilay kapasia.pptxJAYAPATEL52
The document discusses different types of soils found in India. It describes alluvial soil, which is very fertile and found in northern plains, deposited by rivers like the Indus, Ganga and Brahmaputra. It is rich in nutrients. Black soil covers parts of central India and is ideal for cotton. Red or yellow soils are found in southern and eastern parts of the Deccan plateau. Laterite soil, rich in iron but deficient in nutrients, is found in southern states. Arid soil in parts of Rajasthan and Gujarat is saline with low humus. Forest soil in hilly and forest regions is acidic with low humus.
Introduction:
Folding, a fundamental process in structural geology, embodies the dynamic interaction between tectonic forces and the Earth's crust. Understanding the mechanics behind folding is essential for deciphering the deformation history of rock layers and unraveling the complexities of geological structures. This essay explores the mechanics of folding in structural geology, shedding light on the processes that shape the Earth's crust and drive geological evolution.
Fundamental Principles of Folding:
Folding occurs when compressional or extensional forces act upon rock layers, causing them to bend and deform. The mechanical behavior of rocks under stress is governed by principles of elasticity, plasticity, and rheology. Initially, rocks deform elastically, exhibiting reversible strain. However, as stress accumulates, rocks may undergo plastic deformation, resulting in irreversible changes in shape and structure. The rheological properties of rocks, such as their composition, temperature, and pressure conditions, influence their response to deformation and the style of folding observed.
Types of Folds:
Folds manifest in a variety of forms, each reflecting the interplay between tectonic forces and rock properties. Anticlines and synclines represent convex-upward and concave-upward folds, respectively, formed by compressional stresses. Overturned and recumbent folds involve significant tilting of the axial plane, indicating intense deformation. Monoclines and chevron folds exhibit more complex geometries, often associated with localized faulting or folding over basement structures. The diversity of fold types underscores the heterogeneous nature of tectonic processes and the intricate mechanics governing rock deformation.
Factors Influencing Folding:
Several factors influence the mechanics of folding, including the magnitude and direction of tectonic forces, the mechanical properties of rocks, and the presence of pre-existing structures. Convergent plate boundaries, where crustal plates collide, are primary sites of folding and mountain building. Divergent boundaries, characterized by crustal extension, may produce rift-related folding and basin formation. Additionally, the orientation of bedding planes, foliation, and fractures within rock layers can influence the style and orientation of folds.
Deformation Mechanisms:
The mechanisms driving folding include flexural slip, layer-parallel shortening, and buckling. Flexural slip occurs when layers of differing competence within a rock unit slide past each other, leading to the development of hinges and limbs in folds. Layer-parallel shortening involves the contraction of individual layers parallel to their bedding planes, resulting in the development of tight, closely spaced folds. Buckling occurs when compressive forces exceed the elastic limit of rocks, causing them to buckle and fold into characteristic shapes.
Conclusion:
The mechanics of folding in structural geology represent.
India has various types of soil formed by weathering of rocks under different climates and deposition by denudation agents. The six main types are alluvial, black, red, laterite, desert, and mountainous soils. Alluvial soil covers over 7.7 million square km in areas like Uttar Pradesh and covers the most extensive areas. Black soil is best for cotton and found in states like Maharashtra. Red soil covers over 5.18 lakh km2 across central and southern India. Soil erosion due to deforestation, overgrazing, and unscientific farming methods affects soil fertility and agricultural productivity. Conservation methods like terracing, afforestation, check dams, and planned grazing help
Indian soils come in 6 main types - alluvial, laterite, red, black, mountain, and desert soils. Alluvial soils are fertile soils deposited by river sediments. Laterite soils are found in southern India and are rich in iron oxides but less fertile. Red soils develop in low rainfall areas on granite and are moderately fertile. Black soils are very fertile but sticky clay soils found in central India. Mountain soils are humus-rich but low in nutrients. Desert soils are sandy, drain well but lack nutrients and blow away easily. The type of soil depends on climate, vegetation and underlying rock in each region and influences what crops can be grown.
The document discusses laterite soils found in India. Laterite soils are formed in hot, wet, tropical areas through weathering of rocks. They are shallow, acidic soils that are low in fertility. However, they are well suited to growing crops like tea, coffee, and rubber when provided with manure and irrigation. Laterite soils are widely distributed across India, particularly in the southern states of Kerala, Karnataka, Andhra Pradesh, and Tamil Nadu. They have high clay and iron oxide content but are deficient in nutrients like nitrogen.
Soils of India/ Karnataka State New syllabus/ Social Science/ Geography/ Chap...Jaidas Puthan Veetil
Soil is formed by weathering of rocks under different climates and deposited by denudation agents. The main types of soil in India are alluvial soil found in river plains, black soil suited for cotton in central India, red soil covering much of the Deccan plateau, laterite soil in high rainfall areas, desert soil in arid northwest India, and mountain soil rich in nutrients. Soil erosion due to factors like deforestation, overgrazing, and unscientific farming methods needs to be prevented through conservation methods like contour ploughing, bunds, terracing, afforestation, and controlled grazing/irrigation.
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ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
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Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
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How to Add Chatter in the odoo 17 ERP ModuleCeline George
In Odoo, the chatter is like a chat tool that helps you work together on records. You can leave notes and track things, making it easier to talk with your team and partners. Inside chatter, all communication history, activity, and changes will be displayed.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
This slide is special for master students (MIBS & MIFB) in UUM. Also useful for readers who are interested in the topic of contemporary Islamic banking.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
Executive Directors Chat Leveraging AI for Diversity, Equity, and InclusionTechSoup
Let’s explore the intersection of technology and equity in the final session of our DEI series. Discover how AI tools, like ChatGPT, can be used to support and enhance your nonprofit's DEI initiatives. Participants will gain insights into practical AI applications and get tips for leveraging technology to advance their DEI goals.
How to Fix the Import Error in the Odoo 17Celine George
An import error occurs when a program fails to import a module or library, disrupting its execution. In languages like Python, this issue arises when the specified module cannot be found or accessed, hindering the program's functionality. Resolving import errors is crucial for maintaining smooth software operation and uninterrupted development processes.
1. SOIL S OF INDIA
INSTITUTE OF AGRICULTURAL SCIENCES
DEPARTMENT OF AGRONOMY
COURSE- SSC-421 (Soil,Plant,Water &Fertilizer Analysis)
WATER ANALYSIS & SOILS OF INDIA
PRESENTERS-
Prakash kumar (ID-19212AGC101)
UNDER THE SUPERVISION OF
Prof. P K Sharma
Dr. YV Singh
4th Year 8th semester
STUDENT EXPERENTIAL LEARNING
2. Sample collected from Harnuat, Nalanda Bihar
WATER ANALYSIS
9 Water Sample are taken in which only 5 Water Sample consider for testing purpose.
S1, S2, S3, S4, S5 are used in testing purpose.
3. pH & EC-
pH is in the range of 7-8 means slightly alkaline pH, Low EC means
SAMPLE pH (27o) EC (dSm-1)
S1 7.67 0.562
S2 7.40 0.588
S3 7.29 0.802
S4 7.36 0.650
S5 7.22 0.057
low salt good for use.
Carbonate & bicarbonate &
Chloride
CO3- is absent in all sample, Water is moderately soft because
HCO3- Conc is in between 45-80 ppm. Cl- is in b/w 30-115 mg/L
SAMPLE HCO3- (ppm) Cl- (mg/L)
S1 45.75 113.44
S2 67.10 31.196
S3 54.90 59.566
S4 39.65 34.032
S5 51.85 95
Ca & Mg-
Ca+Mg is in between 150-210 ppm means it is hard water.
SAMPLE Ca + Mg (ppm)
S1 208
S2 179.2
S3 86.4
S4 150.4
S5 172.8
Na & K -
Na is in the range of 2-7 ppm & K is in the range1-2 ppm is good for use.
SAMPLE Na(ppm) K(ppm)
S1 6.8 2
S2 3.8 1
S3 4.2 1
S4 2.2 1
S5 4.2 1
4. SOILS OF INDIA-
Loose material and uppermost layer of earth s crust.
Important natural resource.
Formed due to weathering of rocks.
Provides nutrients & water to plants.
Factors affecting soil formation:
Climate
Vegetation
Age of rock
Relief and
Parent rock
5. Classification of Soils
1. In ancient times, Soil was classified into 2 Urvara(Fertile soils) and Usara( Infertile soils).
2. On the basis of colour, composition, characteristic and location, Indian Council of
Agricultural Research (ICAR):
I. Forest Soils
II. Alluvial Soil
III. Desert Soils
IV. Black Soils
V. Laterite Soil
VI. Saline Soils
VII. Red and Yellow Soils
VIII. Peaty Soils
6. Forest Soil
This soil are found in areas with sufficient rainfall and thick forest
They are loamy on valley sides have quality of humus.
In Snow bound areas, soil is acidic and have low humus
They are found in states like Jammu and Kashmir, Uttrakhand, Himachal
Pradesh, Arunachal Pradesh.
7. Alluvial Soil -
•These are soil formed by depositional work of rivers. Example:
Ganga Plain is formed by deposition of alluvium brought by river.
• They are rich in potassium and humus but lack phosphorus and
nitrogen.
• The colour of soil varies from light grey to ash grey.
• They are the most fertile soil and they can be used for the growth
of crops like wheat,rice etc.
• They are found in areas like Indo- Gagnetic plains covering states
of Punjab , Haryana,Uttar Pradesh, Bihar, deltaic region of
Godavari, Krishna and Cauveri.
8. Desert Soil
• This soil is found in areas of high temperature and low rainfall. It is
because of these conditions, the salt get deposited on the top layer
of soil.
• The soil lack nitrogen and humus as it lack vegetation cover and
thus is not suitable for agriculture.
• The colour of the soil varies from red to light brown.
• In this type of soil, kankars are also present
• This soil is found in states like Rajasthan, parts of South-West
Punjab.
9. Black Soil -
1.They are formed by solidification of lava in
Deccan Plateau and therefore rich in minerals.
2.They are clayey in nature,
3.They have capability of storing moisture for a
long time.
4.During rainy season, it becomes sticky and it
becomes difficult to plough. During Summer
season, moisture gets evaporated and deep
cracks appear on the soil.
5.They contain Iron, Aluminum, Potash but lack
nitrogen, phosphorus and organic matter.
6.They are suitable for the growth of cotton.
7.They are found in states like Maharashtra,
Karnataka, Madhya Pradesh and Andhra
Pradesh.
10. Laterite Soil
• These soils are formed by the process of
leaching.
• Leaching is the process by which soil is being
removed due to high temperature and high
rainfall.
• Due to high rainfall, lime and silica are
removed from soil and it is left with iron oxide
and potash.
• The soil lacks organic matter, nitrogen and
calcium.
• The soil becomes hard like brick when dries
and thus is not suitable for agriculture.
• This is found in states like coastal areas of
Karnataka, Kerela ,Tamil Nadu and Assam.
11. SALINE & ALKALINE SOIL —
Contains salts like Sodium, Magnesium, Calcium.
Infertile, unfit for cultivation.
Sandy to loamy in texture. —
Areas: — Parts of Gujarat, Rajasthan, Punjab,
Haryana, U.P & Maharashtra.
12. Red and Yellow Soil
• They are formed due to weathering of
metamorphic rocks.
• They are red in colour due to high iron
in them.
• These soils are rich in potash, iron but lack
lime, phosphate, nitrogen etc.
• With the application of fertilizers, they are
suitable for the growth of wheat and rice.
• They are found in states like parts of
Maharashtra, Karnataka, Chhattisgarh, Odisha,
Jharkhand etc.
13. Peaty Soils
•They are found in areas of high rainfall and
high humidity.
• They are formed due to high vegetation
growth in that area.
• These soils are rich in humus and organic
content.
• They are brown in colour.
• They are found in states like coastal areas of
West Bengal, Odhisha, Tamilnadu.