6 public questions tagged with this topic.
Chlorination of pentane favors the secondary position (C₂/C₄) due to stability, forming CH₃CHClCH₂CH₂CH₃ (2-chloropentane) as the major product.
Ref: NCERT Class 12 Chemistry > Chapter 6: Haloalkanes and Haloarenes > Topic: Classification and Nomenclature and Isomerism of Haloalkanes
Solar energy is the primary source of energy in most ecosystems, as it drives photosynthesis and energy flow.
Ref: NCERT Class 12 Biology Chapter 12: Ecosystem Ecosystem - Structure Components Stratification
The organism is a euglenoid. Euglenoids possess a flexible pellicle and two unequal flagella. They photosynthesise in sunlight but behave as heterotrophs by preying on smaller organisms when sunlight is unavailable.
Ref: NCERT Class 11 Biology Chapter 2: Biological Classification Five Kingdom Classification and Kingdom Plantae Animalia
Deserts are commonly defined by chronic water limitation, and many receive less than about 250 millimetres of precipitation per year. Low rainfall, often combined with high evaporation, prevents continuous tree cover and limits primary productivity. Desert organisms show water-conserving adaptations: plants may use CAM photosynthesis, reduced leaves, succulent tissues, deep or widespread roots, and rapid life cycles after rain; animals may be nocturnal, burrowing, or produce concentrated urine. Not all deserts are hot. Polar and high-altitude deserts can be cold, demonstrating that aridity rather than temperature is the essential criterion. Rainforests and temperate forests need substantially more moisture to maintain closed canopies, while grasslands generally receive intermediate precipitation, often with seasonal drought and fire. The 250-millimetre boundary is approximate because rainfall variability, soil properties, and potential evapotranspiration also determine biological water availability. Even so, among the listed ecosystems, desert most closely matches this annual precipitation threshold. Sparse vegetation then reinforces low productivity and exposes soil to wind and episodic water erosion.
Ref: Ecology: Concepts and Applications, Molles, 9th Ed., Ch. 2-3
The aphotic zone lies below the depth at which usable sunlight can support net photosynthesis. In many aquatic classifications, its upper boundary occurs where irradiance has fallen to about 1% of the value at the surface, although the exact depth changes with water clarity, season, and solar angle. Suspended sediments, dissolved organic matter, and plankton absorb or scatter light, so turbid lakes become aphotic at shallower depths than clear oceans. Because photosynthetic production is negligible there, organisms depend mainly on organic particles sinking from illuminated layers, dissolved organic matter, chemosynthesis in special habitats, or predation. This distinguishes the aphotic zone from the photic or euphotic zone, where enough light remains for photosynthesis, and from the neritic zone, which is defined horizontally as seawater over the continental shelf rather than by illumination. Thus, receiving less than approximately 1% of surface sunlight is the operational ecological feature that identifies aphotic water. Ecologically.
Ref: Ecology: Concepts and Applications, Molles, 9th Ed., Ch. 2-3
Solar radiation supplies most ecosystems because photosynthetic organisms convert a small fraction of incident light into chemical bond energy. That fixed energy enters grazing and detrital pathways and is progressively dissipated as heat through respiration. Heat itself cannot be recycled into biological work at ecosystem temperatures. Exceptions include chemosynthetic communities at hydrothermal vents or subsurface habitats, where oxidation of reduced inorganic compounds powers carbon fixation, but even many apparently dark ecosystems depend on imported photosynthetic organic matter. The amount reaching a consumer level depends jointly on resource production, the fraction consumed, assimilation efficiency, and conversion of assimilates into new biomass. Food-web structure also reflects population persistence: upper levels need enough total production and sufficiently stable prey populations to avoid demographic extinction. Detrital and grazing channels continually exchange material, because waste and mortality feed decomposers while microbial and detritivore biomass supports predators. Quantitative interpretation requires explicit system boundaries and time scales; otherwise export, migration, storage, or seasonal turnover can appear to violate energy balance.
Ref: Fundamentals of Ecology, Odum & Barrett, 5th Ed., Ch. 3
