eChapters

Regeneration capacity of the soil is enhanced with the sowing of MVS which provides ideal condition for regeneration. It creates green cover / dry leaf cover in the top soil (35-40 cm height) which will facilitate the multiplication of inoculated beneficial microbes in the soil.

Multi Varietal seeds sowing techniques

MVS contains seeds of three to four crops belonging to each category viz., cereals, pulses oilseeds, nitrogen fixing green manures and spices and condiments. The seeds of above crops may be mixed in different proportion based on their growth habit and seasonal requirement. For example in the summer the following mixture can be practiced with each of 1-1.5 kg each.

12.1. Problem soils

Chemical constraints: Salinity, sodicity, acidity and nutrient toxicities

Physical constraints : High or low permeability, sub soil hard pan, surface crusting, fluffy paddy soils, sandy soils etc.

10.1. Introduction

The soils possessing characteristics that are not suitable and economical for crop growth are termed as Problem soils. These characteristics may be of physical, chemical and biological. For cultivation of crops in these soils, it is necessary to follow specific management interventions and proper reclamation measures. Frequently we come across another term, ’degraded soil’. Degraded soil is also a problem soil. However, there exists a hair-line difference between problem and degraded soil. Problem soils refer to the soils in which the inherent soil characteristics, obtained from its genesis, pose problems for their optimal use, while degraded soils are developed due to anthropogenic activities by unwise management interventions.

10.2. Types of problem

Mainly there are four types of problem that may exist in soils: physical problems, chemical problems, biological problems and nutritional problems as a result of physical, chemical and biological constraints in soils.

ACID SOILS: Acid soils with pH below 6.5 are widespread. Main limitations of these acid soils are low pH, low CEC, low status of bases, especially Ca, Mg, and K along with toxicity of Al and Mn. Use of acidifying fertilizers aggravates this situation.

Introduction

Problem soils are those that impede agricultural productivity owing to mineral stress, dryness, acidity, sodicity, waterlogging, etc. Vertisol, acid sulphate soils, saline-sodic soils, peat soil, and fine textured alluvial soils were the categories Beek et al., (1980) used to group the problematic soils. In addition to vast areas where deficiencies of zinc, phosphate, and iron, or excesses of iron, aluminium, and manganese limit rice yields, Ikehashi and Ponnamperuma (1978) observed that approximately 100 million hectares of land that are physiographical and climatically suitable for rice lie idle due to the soil toxicities caused by salt, alkali, acid, or organic matter. Problem soils can be broadly defined as those that have unfavourable conditions whether natural or artificially created that severely restrict the successful development of crops. Soil profiles with high groundwater levels and a less permeable argillic layer, degraded soils, sandy soils with low fertility, coastal soils that frequently flood, and laterites could all be categorised as problem soils. Without taking into account related soil functions, soil health is evaluated independently. It is also based on the f indings from a few soil tests for different criteria. 2015 has been recognized the International Year of Soils by the 68th UN General Assembly in recognition of the importance of soil health in all dimensions.

Introduction

Before start of this chapter some pertinent questions need to be answered. What are different agro ecology and what are the problem soils. Since dawn of agriculture in early 2000 B.C. man has been doing agriculture as subsistence farming to cater the needs for his own consumption. Later on as the population increased, the availability of land per pearson reduced and further the commercialization of agriculture after world war II, particularly in industrialized nation, compelled farmers to increase productivity per unit area. The green revolution involving higher fertilizer uses, more use of agrochemicals together with evolvement of improved crop varieties in later part of twentieth century played vital role in producing higher grain production resulting the global production triplet in contrast to merely increase in total global cultivated area to the extent of 10%.

The catastrophe of green revolution was realized in later years when reports of soil health degradation started appearing. Intensified agriculture characterized by excessive use of fertilizers, agrochemicals and unsupportable level of over exploitation of natural resources led to serious degradation of ecosystem. Thus management of agroecosystem has reached to a crossroad with serious pressure to increase productivity simultaneously holding the soil health with prime concern for future generation. Thus the soil heath under different agroecosystem are posing problem as the soil productivity has not reached to plateau level but has started reducing year after year. Thus such soils are becoming problem which need special attention to bring them back to support higher crop production.

The problem soils are those which, due to its land or soil characteristics, cannot be economically used for the cultivation of crops without adopting proper reclamation measures. 
Classification of  Problem Soils:  The problem soils are divided into 3 groups. 
    ·    Highly Eroded Soils 
    ·    Saline and Alkali Soils 
    ·    Acid Soils 
Highly Eroded Soils
These soils are called ‘Usar’ in U.P., ‘Kallar or Thur’ in Punjab and ‘Luni’ in Rajasthan. In India, area under saline alkali soils is 7.0 mha. When the chloride (Cl), sulphate (SO₄^2-), carbonate (CO^₃2-) and bicarbonate(HCO₃-) salts of sodium (Na⁺), calcium (Ca²⁺) and magnesium (Mg²⁺) are increased in the soil, the soil become saline and alkaline. On the basis of amount of soluble salts, average quantity of exchangeable Na and pH, they are classified into 3 groups

The soils which owe characteristics that they cannot be economically used for the cultivation of crops without adopting proper reclamation measures are known as problematic soils. Different kinds of problematic soils viz., Physical, chemical and biological problematic soils exists and pose problems of crop production.

Soil erosion refers to detachment and transport of soil and soil particles from one place to other by the action of water, wind or gravity. Soil erosion consists of (i) detachment of soil particles from surface (ii) their transport from one place to other and (iii) deposition in another place.

Soil erosion are of two types: Natural erosion and accelerated erosion. The natural or geological erosion is steady, nondestructive and slow process of nature. On the contrary the accelerated erosion caused due to human activities like cutting of forest, intensive cropping, construction of roads and building is very rapid and destructive. Surface one inch of soil which is formed in thousand years can be lost within one year due to accelerated erosion.

In India, out of total 175 million hectares of degraded land, soil erosion due to water and wind accounts for 150 million hectare. Soil erosion due to shifting cultivation, salinity, alkalinity, water logging and shifting of water courses account for 25 million hectare.

Average soil loss from various land surfaces in India has been estimated to be 5334 million tonnes per year out of which 29 percent is permanently lost to sea, 10 percent is deposited in reservoirs and 61 percent is transported from one place to other. The plant nutrients lost through 5334 million tonnes of eroded soils was estimated to be 8.4 million tonnes which includes 2.5 million tonnes of N, 3.3 million tonnes of P and 2.6 million tonnes of K.

Siltation of reservoirs through water erosion is a major concern in India. This accelerated silting has considerably reduced the estimated life span of major reservoirs. The rate of siltation depends on the catchment area, soil erodability, topography and rainfall pattern. Larger the catchment area, smaller is the siltation load in the reservoirs because, the coarse fraction of eroded particles may be settle down in the stream valley before the water enters into the reservoir.

Saline and alkali soils occur commonly under arid climate due either to the presence of an excess of soluble sodium salts or to the predominance of sodium among the exchangeable bases.

Saline and alkali soils have been classified as follows

1. Saline soils

Saline soils were originally called “White alkali” soils. Russians term them as “Solonchak” soils.

The soils are classified as saline if the electrical conductivity of saturated soil paste is more than 4 dS /m at 25⁰C, exchangeable sodium is less than 15 percent and pH is less than 8.5.

2. Alkali soils

The soils have been classified as alkali if the electrical conductivity of saturated soil paste is less than 4 dS/m, exchangeable sodium is more than 15 percent and pH is 8.5 to 10.0.

Problems Associated with Rainfed Farming Agriculture

It is a dream desire to eliminate drought from this region. There are many problems that are associated with rainfed farming systems. The problems may be grouped into four major factors: climatic, edaphic, technological and socio- economic.

Climatic

1.Scarcity of rain-water which is low and unpredictable with respect to intensity and distribution;

2.High ET (nearly 3650 mm annually compared to total annual precipitation ranging from 350 to 1400 mm);

3.Extreme thermic values (upto 490C with the mean annual temperature exceeding 180C at some places);

4.High solar incidence (450 to 500 Cal cm² day^-1);

5.High wind velocity with desiccating winds causing a high rate of ET and wind erosion;

6.Low relative humidity;

7.Extensive climatic hazards such as weather aberrations, drought, flood, frost, gale, cyclones and burning winds due to dry, deserted and denuded situations.

Abstract

Development of vermicomposting technology in India was started in seventies, but except some areas of South India it has not been popularized among common masses. This technology is labour intensive and needs attention to handle the tiny earthworms in a proper manner. Sincerity and dedication bring success while casual attitude ends up in financial loss. Lack of proper knowledge on suitable technique, unawareness about nutrient and hygienic standards of vermicompost, non availability of suitable earthworms, lack of marketing and training facility are some major problems in non-flourishing this technology in rural areas. But this technology being simple and easy to follow, is gradually becoming a boon to the low educated poor unemployed youths of the society for their economic development through generating income and creating self employment. Vermicompost, vermi-T and earthworms are marketable product. Government agencies and Non Government Organizations are trying to popularize this technology which has bright prospect to maintain health and hygiene of human to environment.

While developing the toolkit for Participatory Curriculum Development participatory approaches like Focus Group Discussions and Field Level Workshops were adopted. The goal is to provide demand-driven services and to do so, extension professionals need to respond for farmers’ requests rather than deliver predetermined packaged solutions. It is also time to enable the farmers to empower and make their voices heard. Equally important is to make the service providers accountable to the farmers, which is possible when the farmers pay for the services they receive.

4.1 Introduction
Companies that produce tangible items or offer services must drastically increase their productivity in order to maintain their operations in the face of intensifying global competition. A single quantum jump productivity enhancement technique or multiple concurrent incremental improvement productivity strategies can both be used to achieve this goal. If a business chooses the second choice, integrating various tactics for a significant increase in the total productivity would be quite difficult. The first alternative, a single productivity improvement plan, will make it possible for the business to increase productivity with the same or greater success. The only difficulty with this strategy is locating the probable problem area and then using process improvement techniques to achieve the anticipated dramatic increase in productivity. Business process reengineering refers to any significant adjustment of business processes that results in a dramatic increase in an organization’s productivity. Price, quality, after-sales support, adherence to delivery schedules, technological breakthroughs, etc. are some elements that influence market competition. Therefore, the business should focus its efforts on each of these areas in order to achieve notable improvements in terms of decreased operating costs and higher sales revenue from the sale of its goods and services to clients. Improved pricing for a company’s goods or services can provide it an advantage over competitions. Applying various cost-cutting strategies to lower variable costs and overhead costs will lower the price of the good or service. The other elements, viz. quality, after-sales support, delivery schedule adherence, and technological advancements are all directed in this direction

Let‘s dive deeper into the processes of condensation and explore each in more detail:
• Adiabatic Processes: Adiabatic cooling occurs when air rises and expands, reducing its temperature (Fig. 9.1). This process can lead to condensation and cloud formation. There are several ways air can rise and cool adiabatically:
• Orographic Lift: When air is forced to rise over a mountain or hill, it cools, and condensation occurs, resulting in clouds and precipitation. This is why mountainous regions often experience more rainfall than surrounding are as.
• Frontal Lift: When two air masses with different temperatures and humidity levels meet, the warmer air is forced to rise, cool,
and condense, forming clouds and precipitation. This can lead to significant weather changes, such as the formation of fronts and lowpressure systems.
• Convection: When the sun heats the ground, it warms the air closest to the surface, causing it to rise and cool, leading to condensation and cloud formation. This process can lead to the development of cumulus clouds, thunderstorms, and other types of convective weather.

Let’s dive deeper into the processes of condensation and explore each in more detail:
• Adiabatic Processes: Adiabatic cooling occurs when air rises and expands, reducing its temperature (Fig. 10.1). This process can lead to condensation and cloud formation. There are several ways air can rise and cool adiabatically:
• Orographic Lift: When air is forced to rise over a mountain or hill, it cools, and condensation occurs, resulting in clouds and precipitation. This is why mountainous regions often experience more rainfall than surrounding are as.
• Frontal Lift: When two air masses with different temperatures and humidity levels meet, the warmer air is forced to rise, cool,
and condense, forming clouds and precipitation. This can lead to significant weather changes, such as the formation of fronts and lowpressure systems.
• Convection: When the sun heats the ground, it warms the air closest to the surface, causing it to rise and cool, leading to condensation and cloud formation. This process can lead to the development of cumulus clouds, thunderstorms, and other types of convective weather.
• Non-Adiabatic Processes: Non-adiabatic cooling occurs when air cools without rising. There are several ways this can happen:
• Radiation Cooling: When the ground rapidly loses heat by radiation, the air above it cools, and condensation occurs, forming dew, frost, or fog. This process typically occurs overnight, especially in clear skies and calm conditions.

Introduction

GIS (Geographical Information System) based mapping takes cogence of three major geometrical dimensions, point, line and polygons and in GIS these three features correlate their relationship through a concept called Topology. Among the various applications where covariate processing requires specific attention, the landuse/ land cover and Digital Elevation Models/surfaces or terrains are the major area of interest. Use and processing of data for these covariates carries importance as accuracy of both these aspects would influence the derivatives extracted out of them further. For example, if landuse is improperly defined, the site for which planning is proposed may not sustain, similarly, point data/elevation data in case of DEMs would decide the exact topography of any landforms for their further utilization. For their use in GIS, while DEMs depend upon point data, the landuse/ land cover will be taken care by polygons. For the purpose of the study, we are going to discuss about these two covariates in the following paragraphs.

Generally, Covariate (covariable) (koh-vair-iãt) in statistics is defined as a continuous variable that is not part of the main experimental manipulation but has an effect on the dependent variable. In other words, as per ANCOVA (Analysis of covariance) definition: a covariate is a control variable.

Aim of the Experiment: The composite soil samples, collected, are air-dried and processed before analysis in the laboratory.

Introduction
The sun is the primary source of energy for all life on Earth. The primary energy source for the majority of ecosystems is limited to this one. Photosynthesis is performed by green plants, certain types of algae, and microorganisms. They utilize solar energy to fuel chemical reactions that combine basic inorganic components to create intricate organic chemicals. Elements undergo a cyclical process as they move through the different compartments of an ecosystem.
Photosynthesis is the process by which solar energy is captured and transformed into food in the form of chemical energy. Food comprises fundamental elements such as carbon, hydrogen, nitrogen, and other necessary elements, along with stored energy. The components present in the food undergo recycling. The flow of energy and nutrients begins with the producers, then moves to the consumers, and ultimately returns to the producers through the activity of decomposers. Energy, in contrast to materials, is not subject to recycling. Food traverses the food web, resulting in energy dissipation. Typically, just a mere 10% of the energy accumulated in a certain trophic
level, such as the producers, is effectively passed on to the subsequent trophic level, such as the herbivores. This is referred to as the energy pyramid. Ultimately, the energy available in the trophic level becomes so depleted that it cannot sustain any higher trophic levels. Consequently, the presence of fourth order consumers in any ecosystem is extremely rare.
The biotic component, often known as the life component of the environment, encompasses a diverse array of plants, animals, and bacteria, which form interconnected communities.

18.1 Introduction

The farmers have limited resources and a number of enterprises/or enterprise combinations of crops and livestock to choose from. So, the question is how much of what to produce and with what technology. In other words, what combination of enterprises should be produced is expressed as.