{"id":1705,"date":"2014-10-21T11:37:34","date_gmt":"2014-10-21T09:37:34","guid":{"rendered":"http:\/\/www.pasqualerobustini.com\/blog\/?page_id=1705"},"modified":"2020-12-19T13:01:09","modified_gmt":"2020-12-19T12:01:09","slug":"gli-sforzi-principali","status":"publish","type":"page","link":"https:\/\/www.pasqualerobustini.com\/en\/geologia\/elementi-di-geodinamica\/gli-sforzi-principali\/","title":{"rendered":"Principal stresses"},"content":{"rendered":"<p>In structural geology, the analysis of rock deformation in the field or at the microscope (strain analysis) allows us making some assumptions on what kind of stresses had caused those deformations (stress analysis).<\/p>\n<div id=\"attachment_1708\" style=\"width: 372px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-plane-stress.gif\"><img aria-describedby=\"caption-attachment-1708\" class=\"wp-image-1708\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-plane-stress.gif\" alt=\"geodin-plane stress\" width=\"362\" height=\"369\" \/><\/a><p id=\"caption-attachment-1708\" class=\"wp-caption-text\">Tridimensional stress components<\/p><\/div>\n<p>While analyzing stress, it is convenient to describe it within a coordinate system. A 2-dimensional stress has components that are parallel to the x and y axes, that is \u03c3<sub>x<\/sub> e \u03c3<sub>y<\/sub>. The corresponding shear stress will have a component \u03c4<sub>xy<\/sub> (linked to \u03c3<sub>x<\/sub> and parallel to the y axis) and a component \u03c4<sub>yx<\/sub> (linked to \u03c3<sub>y<\/sub> and parallel to the x axis). These are the 4 components of the plane stress (a particular case in which no stress is acting along the z direction, perpendicularly to the xy plane).<\/p>\n<div id=\"attachment_1709\" style=\"width: 373px\" class=\"wp-caption aligncenter\"><img aria-describedby=\"caption-attachment-1709\" class=\"wp-image-1709\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-stress-su-piano.png\" alt=\"geodin-stress su piano\" width=\"363\" height=\"386\" srcset=\"https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-stress-su-piano.png 291w, https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-stress-su-piano-282x300.png 282w\" sizes=\"(max-width: 363px) 100vw, 363px\" \/><p id=\"caption-attachment-1709\" class=\"wp-caption-text\">Stress components on an inclined plane<\/p><\/div>\n<p>The stress upon a plane oriented by an angle \u03b8 with respect to the y axis is represented as in the picture at right. At a certain value of the \u03b8 angle, \u03c3 will reach its maximum value.<\/p>\n<div id=\"attachment_1710\" style=\"width: 478px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-PrincipalStress.gif\"><img aria-describedby=\"caption-attachment-1710\" class=\"wp-image-1710\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-PrincipalStress.gif\" alt=\"geodin-PrincipalStress\" width=\"468\" height=\"271\" \/><\/a><p id=\"caption-attachment-1710\" class=\"wp-caption-text\">Principal stresses<\/p><\/div>\n<p>Around 360\u00b0 there are 2 directions, perpendicular to each other, at which we&#8217;ll have a maximum and a minimum value for the shear stress; stresses perpendicular to those surfaces are called the principal stresses \u03c3<sub>1<\/sub> and \u03c3<sub>2<\/sub>. In these two directions shear stresses are zero.<\/p>\n<p>In three-dimensional stress, the homogeneous stress can always be analyzed in terms of 3 principal stresses perpendicular to each other \u03c3<sub>1<\/sub> \u2265 \u03c3<sub>2<\/sub> \u2265 \u03c3<sub>3<\/sub>, called main, intermediate, and minor principal stress, respectively.<\/p>\n<p>Calculating the stress on a surface whose normal is at a angle \u03b8 from the principal main stress \u03c3<sub>1 <\/sub>can be performed on a diagram where \u03c3 is the x axis and \u03c4 the y axis. All the \u03c3 &#8211; \u03c4 pairs resulting on the different planes while varying the angle \u03b8 from 0 to 360\u00b0 are lying on the so called <strong>Mohr&#8217;s circle<\/strong>.<\/p>\n<div id=\"attachment_1711\" style=\"width: 540px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Mohr_Circle.png\"><img aria-describedby=\"caption-attachment-1711\" class=\"wp-image-1711\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Mohr_Circle.png\" alt=\"geodin-Mohr_Circle\" width=\"530\" height=\"458\" srcset=\"https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Mohr_Circle.png 510w, https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Mohr_Circle-300x259.png 300w\" sizes=\"(max-width: 530px) 100vw, 530px\" \/><\/a><p id=\"caption-attachment-1711\" class=\"wp-caption-text\">Mohr&#8217;s Circles<\/p><\/div>\n<p>The circle intersects the x axis at the values \u03c3<sub>1 <\/sub>and \u03c3<sub>3<\/sub>; its radius is (\u03c3<sub>1 <\/sub>&#8211; \u03c3<sub>3<\/sub>)\/2; its center is at (\u03c3<sub>1 <\/sub>+ \u03c3<sub>3<\/sub>)\/2 and corresponds to \u03c3<sub>2<\/sub>.<\/p>\n<p>Maximum and minimum values of the shear stress are always on two planes at the same angle (\u03b8 \u00b1 45\u00b0) from the main principal stress.<\/p>\n<p>Higher values of shear stress are due to stress differences, not to absolute values of the principal stress. In 3 dimensions, this occurs on two conjugate surfaces which intersect along the intermediate stress axis \u03c3<sub>2<\/sub> at angles of \u00b1 45\u00b0 from \u03c3<sub>1 <\/sub>and \u03c3<sub>3<\/sub>.<\/p>\n<div id=\"attachment_1707\" style=\"width: 458px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Components_of_Stress_Tensor.jpg\"><img aria-describedby=\"caption-attachment-1707\" class=\"wp-image-1707\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Components_of_Stress_Tensor.jpg\" alt=\"geodin-Components_of_Stress_Tensor\" width=\"448\" height=\"355\" srcset=\"https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Components_of_Stress_Tensor.jpg 519w, https:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-Components_of_Stress_Tensor-300x237.jpg 300w\" sizes=\"(max-width: 448px) 100vw, 448px\" \/><\/a><p id=\"caption-attachment-1707\" class=\"wp-caption-text\">The 9 components of the stress tensor<\/p><\/div>\n<p>In different situations from the plane stress, we will have stress components along the z axis. In total, they are the 9 components of the stress tensor, 3 of which are normal to the Cartesian planes: \u03c3<sub>xx<\/sub>, \u03c3<sub>yy <\/sub>and \u03c3<sub>zz<\/sub>.<\/p>\n<p>On planes where the shear stress is zero (\u03c4 = 0) they become the principal stress planes \u03c3<sub>1<\/sub>, \u03c3<sub>2 <\/sub>and \u03c3<sub>3<\/sub>.<\/p>\n<div id=\"attachment_1713\" style=\"width: 347px\" class=\"wp-caption aligncenter\"><a href=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-stress.png\"><img aria-describedby=\"caption-attachment-1713\" class=\"wp-image-1713\" src=\"http:\/\/www.pasqualerobustini.com\/wp-content\/uploads\/2014\/10\/geodin-stress.png\" alt=\"geodin-stress\" width=\"337\" height=\"112\" \/><\/a><p id=\"caption-attachment-1713\" class=\"wp-caption-text\">The 3 principal stresses<\/p><\/div>\n<p>Stress and strain are &#8220;second-order tensors&#8221;. A scalar is a zero-order tensor (one value, no directional properties); a vector is a first-order tensor (value and direction). Second-order tensors define the interactions between vectors and directional operators.<\/p>\n<p>There are 3 perpendicular planes upon which no shear stress acts upon. The same goes for deformation, where we talk about principal strain axes.<\/p>\n<p>&nbsp;<\/p>","protected":false},"excerpt":{"rendered":"<p>In structural geology, the analysis of rock deformation in the field or at the microscope (strain analysis) allows us making some assumptions on what kind of stresses had caused those deformations (stress analysis). While analyzing stress, it is convenient to describe it within a coordinate system. A 2-dimensional stress has components that are parallel to [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1659,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":[],"_links":{"self":[{"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/pages\/1705"}],"collection":[{"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/comments?post=1705"}],"version-history":[{"count":11,"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/pages\/1705\/revisions"}],"predecessor-version":[{"id":6643,"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/pages\/1705\/revisions\/6643"}],"up":[{"embeddable":true,"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/pages\/1659"}],"wp:attachment":[{"href":"https:\/\/www.pasqualerobustini.com\/en\/wp-json\/wp\/v2\/media?parent=1705"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}