Grain sorting is used in the observation of geological specimens such as sands.
Sorting refers to the distribution of grain sizes in a rock.
There are 2 classifications of sorting.
Well sorted = All grains in the rock are the same size. (e.g desert sandstone)
Poorly sorted = A mixture of grain sizes. (e.g Sandstone mixed with clay or gravel mixed with sand)
Well sorted sands result from long transport where unstable minerals have been winnowed out. They have higher porosity and permiability.
Poorly sorted material is the result of rapid deposition of sediment without sorting by currents of wind or water.
more sphericity,more porosity good sorting ,more uniform size and more will be the porosity porosity doesnot depend on size of grain
Three characteristics of a rock's grain include size (fine, medium, coarse), shape (angular, rounded), and sorting (well-sorted, poorly sorted). These characteristics can provide information about the rock's origin and history.
Vertical sorting involves arranging items in a list based on their values in columns, while horizontal sorting involves arranging items in a list based on their values in rows. Both types of sorting help in organizing and analyzing data in a meaningful way.
QuickSort is an unstable sorting technique because it does not guarantee the original order of elements with equal keys. When two elements have the same key, their relative order after sorting is not predictable.
The sorting process used today is often referred to as "comparative sorting" or simply "sorting algorithms." These algorithms, such as QuickSort, MergeSort, and HeapSort, organize data by comparing elements and rearranging them based on specified criteria. In modern applications, sorting is often performed using built-in functions in programming languages, which implement efficient algorithms for optimal performance.
Sediment sorting-Range of particle sizes layering- stratification of sediments and rocks texture- grain size grain Roundness- loss of edges on sediment grains (just took the Quiz of apex!)
Sediment sorting refers to the uniformity of grain size within a deposit, layering refers to the horizontal stratification of sediment, texture describes the size, shape, and arrangement of grains within a sediment, and grain roundness indicates the relative smoothness or angularity of sediment grains.
more sphericity,more porosity good sorting ,more uniform size and more will be the porosity porosity doesnot depend on size of grain
Jo zef Grochowicz has written: 'Machines for cleaning and sorting of seeds =' -- subject(s): Separators (Machines), Grain, Grain-handling machinery, Cleaning
Three characteristics of a rock's grain include size (fine, medium, coarse), shape (angular, rounded), and sorting (well-sorted, poorly sorted). These characteristics can provide information about the rock's origin and history.
The size of the grains in a sedimentary rock can be determined by examining the texture of the rock. Coarser grains indicate a larger grain size, while finer grains indicate a smaller grain size. Other features that can provide clues to grain size include the sorting (uniformity of grain sizes) and rounding of the grains.
Sediment sorting refers to the uniformity of grain sizes in a sediment deposit, with well-sorted sediments having similar-sized grains. Layering refers to the stratification of sediment deposits into distinct layers. Texture refers to the size, shape, and arrangement of grains within a sediment. Grain roundness indicates the degree of abrasion a sediment particle has undergone, with well-rounded grains being smoother and more spherical.
Sorting is the degree of uniformity of grain size of a rock
internal sorting ..............Kaleem
bean, grain, and seed cleaning; corn, peanut, and nut shelling; fruit and vegetable sorting, grading, and cooling; grain, hay, fruit, and vegetable drying; packaging of fresh or farm-dried fruits and vegetables; potato and yam curing
Sorting
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