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A biofertilizer is a substance which contains living micro-organisms which, when applied to seeds, plant surfaces, or soil, colonize the rhizosphere or the interior of the plant and promotes growth by increasing the supply or availability of primary nutrients to the host plant. [1]
Fertilizers are materials that can be added to soil or plants, in order to provide nutrients and sustain growth. Typical organic fertilizers include all animal waste including meat processing waste, manure, slurry, and guano; plus plant based fertilizers such as compost; and biosolids. [2] Inorganic "organic fertilizers" include minerals and ash.
Download as PDF; Printable version; ... and bowl clover. [2] Distribution ... Trifolium cyathiferum is a low growing annual plant. [5]
This biological process, driven by microorganisms such as mycorrhiza and earthworms, releases nutrients available to plants throughout the growing season. Farmers use a variety of methods to improve soil fertility, including crop rotation, cover cropping, reduced tillage, and application of compost.
Trifolium arvense, commonly known as the hare's-foot clover, [1] rabbitfoot clover, [2] stone clover or oldfield clover, is a flowering plant in the bean family Fabaceae. This species of clover is native to most of Europe , excluding the Arctic zone, and western Asia , in plain or mid-mountain habitats up to 1,600 metres (5,200 ft) altitude.
Trifolium repens, the white clover, is a herbaceous perennial plant in the bean family Fabaceae (otherwise known as Leguminosae). It is native to Europe , including the British Isles, [ 2 ] and central Asia and is one of the most widely cultivated types of clover .
"This means clover plants have a symbiotic relationship with soil-dwelling bacteria. The bacteria take nitrogen from the air in the soil and feed it to the clover, keeping it green.
Soil fertility refers to the ability of soil to sustain agricultural plant growth, i.e. to provide plant habitat and result in sustained and consistent yields of high quality. [3] It also refers to the soil's ability to supply plant/crop nutrients in the right quantities and qualities over a sustained period of time.
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