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Dead plant

Detritus Dead plant and animal matter, usually consumed by bacteria, but some remains. [Pg.611]

Saprophytic Bacteria that breakdown bodies of dead plants and animals (nonliving organic material), returning organic materials to the food chain. Saprophytic bacteria are usually non-pathogenic, too. Most Aiken Clear-Flo products are saprophytic. [Pg.625]

Boiler plant operational duties occasionally necessitate starting up boilers from cold (cold plant startups or dead plant startups), bringing a boiler online to support other operational boilers (live plant startups), and taking boilers offline. [Pg.120]

Terrestrial biomass is divided into a number of subreservoirs with different turnover times. Forests contain approximately 90% of all carbon in living matter on land but their NPP is only 60% of the total. About half of the primary production in forests yields twigs, leaves, shrubs, and herbs that only make up 10% of the biomass. Carbon in wood has a turnover time of the order of 50 years, whereas turnover times of carbon in leaves, flowers, fruits, and rootlets are less than a few years. When plant material becomes detached from the living, plant carbon is moved from the phytomass reservoir to litter. "Litter" can either refer to a layer of dead plant material on the soil or all plant materials not attached to a living plant. A litter layer can be a... [Pg.293]

Besides nitrogen fixation, the only other major source of reduced nitrogen is the decomposition of soil or aquatic organic matter. This process is called ammonification. Heterotrophic bacteria are principally responsible for this. These organisms utilize organic compounds from dead plant or animal matter as a carbon source, and leave behind NH3 and NHJ, which can then be recycled by the biosphere. In some instances heterotrophic bacteria may incorporate a complete organic molecule into their own biomass. The majority of the NH3 produced in this way stays within the biosphere however, a small portion of it will be volatilized. In addition to this source, the breakdown of animal excreta also contributes to atmospheric... [Pg.327]

Clays occur naturally either in a relatively pure condition or mixed with other materials and they are therefore classified into one of two large groups primary and secondary clays. Primary clays are quite pure, uncontaminated by other materials, and have a rather uniform composition. Secondary clays are mixtures of clay with other minerals such as quartz, talc, mica, iron oxides, and even organic matter (the latter derived from the decay of dead plants and animals) the particles of most of the contaminating materials are generally of similar size to those of the clay (Kingery et al. 1976). [Pg.258]

A high amount of various nutrients and trace metals is retained in peat and dead plant residues and thus temporarily eliminated from the biogeochemical cycles and pollutants exposure to human and ecosystem health. The period of this elimination depends on the solubility of these metals. It has been shown (Dobrovolsky, 1994) that... [Pg.130]

The biomass of Tundra ecosystems gradually increases from 4-7 ton/ha for moss-lichen tundra to 28-29 ton/ha by dry weight for low-bush tundra. In the northern tundra, the plant biomass and dead organic matter are eventually shared. Southwards this percentage tends to diminish, and low-bush living biomass is smaller than dead plant remains mass. A typical feature of the Tundra ecosystems plant species is the prevalence of underground matter (roots) up to 70-80% of the total biomass. [Pg.134]

The half-life of the process in Equation (8.32) is 5570 years. Following death, flora and fauna alike cease to breathe and eat, so the only 14C in a dead body will be the 14C it died with. And because the amounts of 14C decrease owing to radioactive decay, the amount of the 14C in a dead plant or person decreases whereas the amounts of the 12C and 13C isotopes do not. We see why the proportion of 14C decreases steadily as a function of time following the instant of death. [Pg.384]

Many bacteria perform services we find useful and even necessary, although we rarely take note of them. Some bacteria participate in the decomposition of dead plants and animals and so help recycle chemicals that are otherwise locked away from the living world. Some are sources of antibiotics that have revolutionized the treatment of infectious disease in the past fifty years. Others are responsible for nitrogen fixation, converting relatively inert atmospheric nitrogen into biologically useful ammonia—a conversion that is not simple in the chemical laboratory. Still other bacteria are indispensable in the world s kitchens, for without them there would be no cheese or yogurt, nor any of hundreds of other traditional milk products. We could not enjoy pickles or sauerkraut, and... [Pg.124]

To understand this, something must first be said about the typical characteristics and profile of soil. Soil is made of mineral particles including sand, silt, and clay, as well as living and dead plants and animals (organic matter), air, and water. But differing layers of soil, at differing depths, have different mixes and densities of these materials. Soils are layered with differing Horizons stacked on top of one another, usually identified from the so-called A Horizon (near the... [Pg.39]

Dispose of dead plants, or those badly infected with pests or disease, immediately. [Pg.250]

Susceptible plants Most living or dead plant material. [Pg.330]

Likewise, WoodwelPs prediction" of enhancement of the activity of insect pests and some disease agents (which has been demonstrated in the San Bernardino Mountains forest) could lead to an increase in vertebrate species that feed on invertebrates or utilize dead plants for cover. Birds would be the most likely to increase and, to a lesser extent, such small mammals as deer mice, which are partially insectivorous. [Pg.631]

Collins believes that we can get the things we need out of recently dead plant matter rather than fossilized plant matter, and this is an active area of industrial research. [Pg.32]

How does one know whether a body of water is polluted In some cases, the answer to that question is easy. Just looking at a river or stream sometimes reveals the presence of dead plants and animals, discarded tires and plastic bottles, oil films, and other obvious evidence of pollution. But detecting pollution is not always that easy. Water that looks crystal clear and pure may sometimes harbor disease-causing organisms, toxic chemicals, or other materials that make It unsafe to drink or use. One of the pioneers in developing methods for detecting water pollution is Ruth Patrick. [Pg.112]


See other pages where Dead plant is mentioned: [Pg.418]    [Pg.838]    [Pg.354]    [Pg.663]    [Pg.244]    [Pg.303]    [Pg.29]    [Pg.101]    [Pg.1458]    [Pg.1508]    [Pg.236]    [Pg.132]    [Pg.182]    [Pg.21]    [Pg.465]    [Pg.82]    [Pg.64]    [Pg.44]    [Pg.216]    [Pg.217]    [Pg.6]    [Pg.636]    [Pg.358]    [Pg.315]    [Pg.102]    [Pg.105]    [Pg.219]    [Pg.278]    [Pg.101]    [Pg.1458]    [Pg.1508]    [Pg.46]    [Pg.46]    [Pg.60]   
See also in sourсe #XX -- [ Pg.14 , Pg.229 , Pg.246 , Pg.247 , Pg.257 , Pg.269 , Pg.279 , Pg.296 ]




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Chemical differences between living and dead plants

DEAD

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Deadly nightshade plant

Plant dead volume

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