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Soil gases (soil atmosphere [1]) are the gases found in the air space between soil components. The spaces between the solid soil particles, if they do not contain water, are filled with air. The primary soil gases are nitrogen, carbon dioxide and oxygen. [2] Oxygen is critical because it allows for respiration of both plant roots and soil ...
Aerenchyma in stem cross section of a typical wetland plant. Aerenchyma or aeriferous parenchyma [1] or lacunae, is a modification of the parenchyma to form a spongy tissue that creates spaces or air channels in the leaves, stems and roots of some plants, which allows exchange of gases between the shoot and the root. [2]
Gas exchange is the physical process by which gases move passively by diffusion across a surface. For example, this surface might be the air/water interface of a water body, the surface of a gas bubble in a liquid, a gas-permeable membrane, or a biological membrane that forms the boundary between an organism and its extracellular environment.
Cuticles can also reflect light, like trichomes, which reduces light intensity and heat. Plant cuticles can also limit the diffusion of water and gases from the leaves which helps maintain them under stress conditions. Thicker cuticles have been found to decrease evaporation, so some plants will increase the thickness of their cuticles in ...
C3 plants do not grow well in very hot or arid regions, in which C4 and CAM plants are better adapted. The isotope fractionations in C3 carbon fixation arise from the combined effects of CO 2 gas diffusion through the stomata of the plant, and the carboxylation via RuBisCO. [1] Stomatal conductance discriminates against the heavier 13 C by 4.4 ...
Soil texture and structure strongly affect soil porosity and gas diffusion. It is the total pore space of soil, not the pore size, and the degree of pore interconnection (or conversely pore sealing), together with water content, air turbulence and temperature, that determine the rate of diffusion of gases into and out of soil.
One problem in the measurement of soil respiration in the field is that respiration of microorganisms can not be distinguished from respiration from plant roots and soil animals. This can be overcome using stable isotope techniques. Cane sugar is a C 4 – sugar which can act as an isotopic tracer.
The pineapple is an example of a CAM plant.. Crassulacean acid metabolism, also known as CAM photosynthesis, is a carbon fixation pathway that evolved in some plants as an adaptation to arid conditions [1] that allows a plant to photosynthesize during the day, but only exchange gases at night.