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SOIL FERTILITY
Soil scientists that focus on soil fertility are interested in managing nutrients to improve crop production. They focus on using commercial fertilizers, manures, waste products, and composts to add nutrients and organic matter to the soil. Sometime they also add chemicals that change the pH to a more optimum level for nutrient availability to plants. Soil fertility experts must also be careful to ensure that practices are environmentally sustainable. Inappropriate management of nutrients can lead to contamination of lakes, rivers, streams, and groundwater. In addition, adding amendments to the soil is expensive and cuts into the profitability of farming operations, not to mention that toxic levels of nutrients can be as bad as or worse than too little nutrients for the plants.
Nutrient Deficiencies
There are 17 essential plant nutrients, three come from air and water (carbon, oxygen, and hydrogen) and 14 come from the soil. The table below describes the essential and beneficial elements obtained from the soil. Macronutrients are needed in high quantity, micronutrients are needed in small amounts, and beneficial elements are essential or beneficial to some plants, but not all.
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Nitrogen | N | NO , NH | Protein and enzyme component | General yellowing of leaves, stunted growth, often older leaves affected first. |
Phosphorus | P | HPO , HPO | Membranes, energy, DNA | Difficult to visualize until severe. Dwarfed or stunted plants. Older leaves turn dark green or reddish-purple. |
Potassium | K | K | Osmotic balance | Older leaves may wilt or look burned. Yellowing between veins begins at the base of leaf and goes inward from the leaf edges. |
Calcium | Ca | Ca | Cell structure | Fruit/flower and new leaves are distorted or irregular. When severe, leaves will be necrotic near the base. Leaves can be cupped downward. Occurs more often at low pH. |
Magnesium | Mg | Mg | Chlorophyll, enzyme activation | Older leaves will turn yellow and brown around the edge of the leaf leaving a green center. May appear puckered. Occurs more often at low pH. |
Sulfur | S | SO | Protein and enzyme component | Yellowing leaves starts with younger leaves. |
| | | | |
Iron | Fe | Fe , Fe | Enzyme function, required for chlorophyll production | Yellowing between veins that start with younger leaves. Occurs more often at high pH. |
Manganese | Mn | Mn | Enzyme component | Yellowing between veins that start with younger leaves. Pattern is not as distinct as with Fe deficiency, may appear in patches or freckled. Occurs more often at high pH. |
Zinc | Zn | Zn | Enzyme component | Yellowing between veins of younger leaves. Terminal leaves may be rosette. Occurs more often at high pH. |
Boron | B | H BO | Cell wall | Terminal buds die. Light general yellowing. B requirements are very plant specific. |
Copper | Cu | Cu | Enzyme function | Dark green stunted leaves. Curled leaves often bend downwards. Sometimes wilted with light overall yellowing of leaves. Occurs more often at high pH. |
Molybdenum | Mo | MoO | Enzyme function | Yellowing of older leaves and light green rest of the plant. It usually appears as N deficiency due to role in nitrate assimilation and in legumes in N-fixing bacteria. Occurs more often at low pH. |
Chlorine | Cl | Cl | Osmotic balance, plant compounds | Almost never deficient. Abnormally shaped leaves; Yellowing and wilting of young leaves. |
Nickel | Ni | Ni | Enzyme component | Almost never deficient. |
| | | |
Silicon | Si | | increased pest and pathogen resistance, drought resistance, heavy metal tolerance, higher quality and yield of crop |
Cobalt | Co | Co | Required for N-fixation by bacteria associated with legumes |
Sodium | Na | Na | Required for photosynthesis in C4 and CAM species adapted to warm climates |
Soil Test Interpretations
There are many factors to consider when producing a crop or growing a garden. How much fertilizer to apply and when to apply it are some of the decisions that must be made. These decisions depend on the crop to be grown, the soil type, and the environmental conditions under which it is grown. Soil testing laboratories associated with universities have conducted years of field and greenhouse research with various crops and soils to determine how a particular crop responds to soil test levels of plant nutrients. Most laboratories use a rating scale that includes “Low”, “Medium”, “High”, and “Very High” to describe the soil test level of a particular nutrient for a particular crop in a particular soil type. When a nutrient level is low or very low level, a fertilizer containing that nutrient is usually recommended. Once a soil test rating reaches “High” or “Very High”, then the grower can save money by not applying any more of that nutrient. By not applying when soil test levels are high and by creating rating scales that are specific to general soil types, the environment can be protected from excessive nutrients.
Nutrient Management
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Soil Fertility: Replenishment Of Nutrients
What is soil fertility.
“Soil fertility refers to the ability of the soil to sustain plant growth.”
Fertile soil results in high yield and better quality of plants. Fertile soil is rich in fundamental elements and minerals, has good aeration, water holding capacity, and good texture.
Let us have a look at what is soil fertility and how can it be replenished.
Factors Affecting Soil Fertility
The following factors affect the soil fertility:
Mineral Composition
The mineral composition of the soil helps to predict the ability of the soil to retain plant nutrients. Application of proper fertilizers and manures helps in enhancing the quality of the soil.
Soil pH helps in maintaining the nutrient availability of the soil. A pH range between 5.5-7 is optimum for soil fertility.
Soil Texture
The minerals of different sizes are responsible for maintaining the structure of the soil. Clayey soil can retain more nutrients and hence acts as a nutrient reservoir.
Organic Matter
Organic matter is a source of nitrogen and phosphorus. These can be mineralized and made available to the plants.
Also Read: Biofertilizers
Nutrient Replenishment
Nutrients can be replenished in the following ways:
Adding Manures and Fertilizers
Fertilizers such as nitrogen, potassium and phosphorus are added to the soil to make it fertile. These are also added to the potted plants in gardens to enhance plant growth. NPK and urea are the most common fertilizers required by the soil. Urea adds nitrogen to the soil. Whereas, NPK adds nitrogen, potassium and phosphorus to the soil.
Leguminous Crops
Leguminous plants contain nitrogen-fixing bacteria such as Rhizobium in the root nodules. These bacteria trap atmospheric nitrogen and make it available to the plants in the form of nitrogen compounds. The remaining nitrogen compounds are mixed with the soil to increase its fertility.
Also Read: Rhizobium
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Soil Fertility
An introduction to soil fertility.
Just like humans, crops also require nutrients. Fertile soil contains all of the major nutrients required for basic plant nutrition (For example, nitrogen, phosphorus, and potassium), as well as other nutrients required in smaller amounts (For example, calcium, magnesium, sulfur, iron, zinc, copper, boron, molybdenum, nickel).
This article gives insight into what is fertile soil and its importance, the types of fertile soil, the principles of soil fertility and what are the various majors that can be taken to increase soil fertility.
Soil fertility can be defined as the ability of the soil to provide an atmosphere that is in favour of plant growth . It refers to the soil's ability to support plant growth and maximise crop yield. This can be improved by applying organic and inorganic fertilisers to the soil. Nuclear techniques provide information that improves soil fertility and crop production while reducing environmental impact.
This includes providing the plant with the essential nutrients and a suitable chemical, a physical and biological environment that enhances and promotes the growth of a plant. Fertile soil will typically have some organic matter that improves soil structure, moisture retention, and nutrient retention, as well as a pH between 6 and 7. Unfortunately, many soils lack adequate levels of all essential plant nutrients or soil conditions are unfavourable for plant uptake of certain nutrients.
Soil fertility and plant nutrition focus on the management of essential elements that are necessary for plant growth. Soil fertility directly affects the quality as well as the quantity of the crop production affecting how it can be further used for human uses. A single element is also considered essential if it is required for plant metabolism and the completion of the plant’s life cycle.
There are 17 elements that meet these criteria and are divided into macro and micronutrients . This, along with the composition of the plant, forms the biology and fertility of soils.
Types of Soil Fertility
Inherent or Natural Fertility:
The soil that naturally contains some nutrients and is considered fertile is known as inherent fertility. Some of the nutrients like nitrogen, phosphorus and potassium are considered essential for the normal growth and yield of the crop. These are naturally present in naturally fertile soil. The inherent fertility has a limiting factor from which fertility is not decreased.
Acquired Fertility:
When the fertility of the soil is developed through external agents like manures and fertilisers, tillage, irrigation etc., it is known as acquired fertility. It has been found that the yield does not increase after a point by the application of an additional quantity of fertilisers. Thus, this becomes the limiting factor of acquired fertility.
Soil Fertility and Fertilisers
Fertilisers are mixtures of nitrogen, phosphorus, and potassium compounds that promote plant growth. Fertilizers that provide all three elements are frequently referred to as NPK fertilisers, after the chemical symbols for these three elements. Inappropriate or excessive fertilisation can be harmful to the ecosystem , but it is necessary to produce adequate food for the growing population . Overuse or repeated use of fertilisers can result in an ultimate decrease in soil fertility along with acidification of the soil.
It will gradually decrease the amount of organic matter, humus and beneficial organisms in the soil which will lead to inhibiting plant development, altering soil pH, increasing pests and even releasing greenhouse gases. Fertilisers are not meant for continuous or constant use as they can result in the overall infertility of the soil in the long term. This kind of soil will not be safe to use in future for any kind of crop production.
Importance of Soil Fertility
Soil starts the chain of the food cycle wherein it feeds the plant which ultimately feeds us. They are the primary organisms of the food chain. With the improvement of soil, there will be a gradual increase in the quality of plant and crop production as well. Some of the essential aspects of soil fertility are described below:
Soil provides direct nutrition and a foundation for plants . It is considered the most important factor in determining plant growth.
Soil is a result of the accumulation of decomposing plant and animal matter with the ageing parent material. As this soil breaks down, these elements are released in the form of nutrients that are directly available to the growing plant.
How to Increase Soil Fertility?
There are a few ways in which one can increase soil fertility or replenish the nutrients removed from the soil. Some of these are discussed below:
Recycling Nutrients: This can be done by the use of plant and animal waste.
Use of fertilisers.
Through Microbial Action: This includes the use of nitrogen fixation which can be achieved through the use of grain legumes that initiates biological nitrogen fixation. This can also be done by other methods like fertilisers, green manures, etc.
Incorporating Cover Crops: Using cover crops can add organic matter to the soil improving soil fertility and making it healthy for plant production.
In this article, we have studied about natural and acquired fertility of the soil and how we can improve the soil by adding compost and rotating crops every year. A fertile soil's primary function is to provide food, which is critical in light of the FAO's Zero Hunger goal. A fertile soil also provides essential nutrients for plant growth, resulting in healthy food that contains all of the nutrients required for human health. Fertile soil is typically found in river valleys or areas where glaciers deposited minerals during the last Ice Age. Mountains are usually less fertile than valleys and plains.
FAQs on Soil Fertility
1. What is leaching and how does it affect soil fertility?
Leaching is a process due to which the soil loses its water-soluble nutrients and colloids from the top layer. This might happen due to rain or irrigation. Due to this process, these nutrients are carried downward (eluviated) and are generally redeposited (illuviated) in a lower layer of the soil resulting in an open top layer and a dense, compact lower layer.
One of the elements that are a vital nutrient for plant growth is boron. Leaching can affect water soluble boron and cause deficiencies in the crops. A deficiency of boron from the crops can result in diseases with visual symptoms of misshapen, thick, brittle, small leaves.
2. How important is the chapter Increasing soil fertility from CBSE’s point of view?
The chapter on increasing soil fertility is considered one of the most important chapters from an examination point of view. It has to be covered thoroughly while remembering the major points. The chapter covers topics that involve factors affecting soil fertility and how to improve it, the macro and micronutrients involved in plant growth and production. It also talks about topics like fertilisers and how it affects soil fertility.
3. When should one fertilise their plants?
Fertiliser is most effective when applied to plants during their active growth cycle. For deciduous species, this is when the plant begins to leaf out, flower, or put on new growth after emerging from the dormant winter stage. The best time of year to fertilise most plants is in the spring. Vegetable gardeners can use a quick-release fertiliser once a month or a slow-release fertiliser once a season to fertilise their garden beds. Some gardeners prefer to feed their flowers and plants once every one to two weeks with a portion of liquid-soluble plant food.
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Nickel and soil fertility: review of benefits to environment and food security.
1. Introduction
2. the role of ni in soil fertility and the plant-rhizosphere environment, 3. transport and accumulation of ni in plants, 4. nickel and biotic stress in plants, 5. advancement in ni delivery to plants and future research, 6. discussion, 7. conclusions, author contributions, conflicts of interest.
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Click here to enlarge figure
Deficiency | Related Macronutrient | Crop | Damage to Crop | Ref |
---|
Bitter pit | Ca | apple | lower fruit value, decreased fruit shelf life | [ ] |
Blossom end rot | Ca | tomato (Solanum lycopersicum), bell pepper (Capsicum annuum), eggplant (Solanum melongena) | loss of fruit due to tissue damage | [ ] |
Diminished seed viability | N/A | all seed-bearing plants | poor seed development | [ ] |
Mouse-ear | urea-N | pecan, hazelnut | urea toxicity damage to leaf | [ ] |
Model Crop | Fungal Diseases | Application (Estimated kg ha ) | Effect | Refs |
---|
Cherry | Leaf spot (Alternaria alternaria) | 0.125 | 50–60% less leaf spot | [ ] |
Daylily | Daylily rust (Puccinia hemerocallidis) | N/A, 200 mg L | 90% reduction | [ ] |
Lettuce, Tomato | Fusarium wilt (F. oxysporum f. sp. lactucae and F. oxysporum f. sp. lycopersici) | N/A, nickel nanoparticles 100 ppm | 30–60% growth inhibition | [ ] |
Pecan | Pecan scab (Fusicladium effusum G. Winter) | 0.05–0.1 | reduces leaf lesions by 50% | [ ] |
Soybean | Asian soybean rust (Phakopsora pachyrhizi) | 0.075 | lowers severity by 35% | [ ] |
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Share and Cite
Rabinovich, A.; Di, R.; Lindert, S.; Heckman, J. Nickel and Soil Fertility: Review of Benefits to Environment and Food Security. Environments 2024 , 11 , 177. https://doi.org/10.3390/environments11080177
Rabinovich A, Di R, Lindert S, Heckman J. Nickel and Soil Fertility: Review of Benefits to Environment and Food Security. Environments . 2024; 11(8):177. https://doi.org/10.3390/environments11080177
Rabinovich, Alon, Rong Di, Sean Lindert, and Joseph Heckman. 2024. "Nickel and Soil Fertility: Review of Benefits to Environment and Food Security" Environments 11, no. 8: 177. https://doi.org/10.3390/environments11080177
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Environmental Drivers of Soil Organic Carbon in the Australian Rangelands
24 Pages Posted: 22 Aug 2024
Mingxi Zhang
Curtin University
Soil organic carbon (SOC) is vital for maintaining healthy ecosystems and providing various benefits beyond climate change mitigation. These benefits include supporting biodiversity and improving nutrient cycling, fertility and soil structure. This study aims to investigate the environmental drivers of SOC content across the vast Australian rangelands at different spatial scales. We describe the state of SOC as a function of a large set of soil and environmental variables, representing factors that represent soil mineralogy, climate, vegetation, topography, and soil microbial diversity. We used a quantitative hierarchical framework over three distinct climate zones to gain a systematic understanding of the controls of SOC variability at a macro, regional and local scale. Over the macro-scale of the rangelands, we find that climate is the dominant control of SOC in the Australian rangelands and influences SOC both directly and indirectly through its effects on vegetation growth. At the regional scale, the distribution of SOC is largely determined by regional controls such as soil texture and mineralogy and microbial diversity, vegetation cover and type and plant species richness, and local terrain features. At a local transect scale, SOC variability is affected by vegetation type and biomass, terrain attributes (terrain wetness index, plan curvature and erosion), soil mineralogy and microbial diversity. At these local scales, where plant carbon inputs are not limited by climate, vegetation type is the most significant driver. Where plant carbon inputs are limited by climate, SOC is controlled by vegetation biomass and type and soil mineralogy. Vegetation with shallow roots and limited soil development, contributes minimal carbon to the subsoil, whereas deep-rooted vegetation, less limited by climate, sequesters significant carbon. Our results provide insights into the drivers of SOC content in Australian rangelands and could serve to develop strategies for long-term SOC sequestration and restoration.
Keywords: Soil organic carbon, Environmental drivers, Spatial scales, Soil depth, Rangelands
Suggested Citation: Suggested Citation
Mingxi Zhang (Contact Author)
Curtin university ( email ).
Kent Street Bentley Perth, WA 6102 Australia
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COMMENTS
Soil productivity encompasses soil fertility plus the inherent and management-related factors affecting plant growth and development. It is generally measured in terms of inputs versus outputs, which for agronomic situations generally refers to water and/or nutrient input versus crop yield.
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These benefits include supporting biodiversity and improving nutrient cycling, fertility and soil structure. This study aims to investigate the environmental drivers of SOC content across the vast Australian rangelands at different spatial scales. We describe the state of SOC as a function of a large set of soil and environmental variables ...
Soil Fertility - Science topic Explore the latest questions and answers in Soil Fertility, and find Soil Fertility experts.
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