{"id":3304,"date":"2026-10-22T19:08:43","date_gmt":"2026-10-22T19:08:43","guid":{"rendered":"https:\/\/dlhb.art\/?p=3304"},"modified":"2026-10-22T19:08:43","modified_gmt":"2026-10-22T19:08:43","slug":"22-10-26","status":"publish","type":"post","link":"https:\/\/dlhb.art\/da\/22-10-26\/","title":{"rendered":"22\/10\/26"},"content":{"rendered":"<p class=\"wp-block-paragraph\">If\u00f8lge vores eneste jordpr\u00f8ve, der er blevet analyseret p\u00e5 et laboratorium, er vores jordtype en lerholdig sandjord med 88% sand, 6% silt og 4% ler. If\u00f8lge analyserapporten har jorden ikke tendens til tilslemning. P\u00e5 grund af de h\u00e5rde, bare jordomr\u00e5der var jeg i tvivl om, hvorvidt jordtypen andre steder adskiller sig fra den ved pr\u00f8veudtagningsstedet. Derfor begyndte jeg at udtage jordpr\u00f8ver forskellige steder p\u00e5 gr\u00e6smarken og unders\u00f8ge de lag, der dannes, ved hj\u00e6lp af den s\u00e5kaldte sedimentationstest.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">Med fingrene kan man rulle ler ud til en p\u00f8lse, der er cirka halvt s\u00e5 tyk som en blyant. Sandfraktionen kan derimod ikke rigtig rulles ud.<\/p>\n\n\n\n<figure class=\"wp-block-gallery has-nested-images columns-default is-cropped wp-block-gallery-1 is-layout-flex wp-block-gallery-is-layout-flex\">\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"769\" height=\"1024\" data-id=\"3306\" src=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-769x1024.jpg\" alt=\"\" class=\"wp-image-3306\" srcset=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-769x1024.jpg 769w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-225x300.jpg 225w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-767x1022.jpg 767w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-1153x1536.jpg 1153w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-9x12.jpg 9w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-1538x2048.jpg 1538w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-600x799.jpg 600w\" sizes=\"auto, (max-width: 769px) 100vw, 769px\" \/><figcaption class=\"wp-element-caption\">Jordpr\u00f8ve udtaget under gr\u00e6sset<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"769\" height=\"1024\" data-id=\"3309\" src=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-769x1024.jpg\" alt=\"\" class=\"wp-image-3309\" srcset=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-769x1024.jpg 769w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-225x300.jpg 225w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-767x1022.jpg 767w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-1153x1536.jpg 1153w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-9x12.jpg 9w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-1538x2048.jpg 1538w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252578-1-600x799.jpg 600w\" sizes=\"auto, (max-width: 769px) 100vw, 769px\" \/><figcaption class=\"wp-element-caption\">Fraktioner fra de enkelte lag i \u00bbgr\u00e6spr\u00f8ven\u00ab. Is\u00e6r i den midterste fraktion kan man se et h\u00f8jt indhold af organisk materiale.<\/figcaption><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"769\" height=\"1024\" data-id=\"3310\" src=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-769x1024.jpg\" alt=\"\" class=\"wp-image-3310\" srcset=\"https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-769x1024.jpg 769w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-225x300.jpg 225w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-767x1022.jpg 767w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-1153x1536.jpg 1153w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-1538x2048.jpg 1538w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-9x12.jpg 9w, https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792691068694-1-600x799.jpg 600w\" sizes=\"auto, (max-width: 769px) 100vw, 769px\" \/><figcaption class=\"wp-element-caption\">Af de delvist t\u00f8rrede fraktioner fra pr\u00f8ven, der blev taget p\u00e5 det bare jordomr\u00e5de, kan man forme sm\u00e5 p\u00f8lser (sandet er allerede blevet sorteret fra). \u00d8verst lerholdigt materiale, nederst sandsynligvis silt.<\/figcaption><\/figure>\n<\/figure>\n\n\n\n<p class=\"wp-block-paragraph\">De tre jordpr\u00f8ver, der hidtil er blevet udtaget, stammer fra en h\u00e5rd jordklump fra komposten, et h\u00e5rdt sted p\u00e5 marken og et sted med t\u00e6t gr\u00e6sv\u00e6kst. Der ses ingen st\u00f8rre forskel i lagdannelsen.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">I pr\u00f8ven fra det gr\u00e6skl\u00e6dte omr\u00e5de var vandet stadig ikke blevet helt klart, selv efter fem dage. Det kan muligvis skyldes et h\u00f8jt indhold af organisk materiale. F\u00f8r jeg tog denne pr\u00f8ve, fjernede jeg gr\u00e6slaget med en spade, men jeg gravede \u00e5benbart ikke dybt nok (kun ca. 6 cm).<\/p>\n\n\n\n<p class=\"wp-block-paragraph\">I alle pr\u00f8ver var laget af silt og ler omkring en halv centimeter tykt, mens sandlaget udgjorde ca. 6 cm. Der synes alts\u00e5 ikke at v\u00e6re steder med markant h\u00f8jere indhold af silt eller ler.<\/p>\n\n\n\n<p class=\"wp-block-paragraph\"><\/p>","protected":false},"excerpt":{"rendered":"<p>Laut unserer einzigen durch ein Labor ausgewerteten Bodenprobe ist unsere Bodenart ein lehmiger Sand mit 88% Sand, 6% Schluff und 4% Ton. Laut Analysebericht neigt der Boden nicht zur Verschl\u00e4mmung. Aufgrund der harten, offenen Bodenstellen hatte ich Zweifel, ob die Bodenart an anderen Stellen von der an der Probenahmestelle abweicht. Daher habe ich begonnen, an [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":3306,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"_uag_custom_page_level_css":"","site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"set","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[127],"tags":[123,126,125,124,122],"class_list":["post-3304","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-boden","tag-bodenart-bestimmen","tag-bodenverdichtung","tag-fingerprobe-boden","tag-sand-schluff-ton","tag-schlaemmprobe-boden"],"uagb_featured_image_src":{"full":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693.jpg",3472,4624,false],"thumbnail":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-150x150.jpg",150,150,true],"medium":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-225x300.jpg",225,300,true],"medium_large":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-767x1022.jpg",767,1022,true],"large":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-769x1024.jpg",769,1024,true],"1536x1536":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-1153x1536.jpg",1153,1536,true],"2048x2048":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-1538x2048.jpg",1538,2048,true],"trp-custom-language-flag":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-9x12.jpg",9,12,true],"woocommerce_thumbnail":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-300x300.jpg",300,300,true],"woocommerce_single":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-600x799.jpg",600,799,true],"woocommerce_gallery_thumbnail":["https:\/\/dlhb.art\/wp-content\/uploads\/2026\/10\/1792690252693-100x100.jpg",100,100,true]},"uagb_author_info":{"display_name":"dlhb@netmail.dk","author_link":"https:\/\/dlhb.art\/da\/author\/dlhbnetmail-dk\/"},"uagb_comment_info":0,"uagb_excerpt":"Laut unserer einzigen durch ein Labor ausgewerteten Bodenprobe ist unsere Bodenart ein lehmiger Sand mit 88% Sand, 6% Schluff und 4% Ton. Laut Analysebericht neigt der Boden nicht zur Verschl\u00e4mmung. Aufgrund der harten, offenen Bodenstellen hatte ich Zweifel, ob die Bodenart an anderen Stellen von der an der Probenahmestelle abweicht. Daher habe ich begonnen, an&hellip;","_links":{"self":[{"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/posts\/3304","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/comments?post=3304"}],"version-history":[{"count":4,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/posts\/3304\/revisions"}],"predecessor-version":[{"id":3314,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/posts\/3304\/revisions\/3314"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/media\/3306"}],"wp:attachment":[{"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/media?parent=3304"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/categories?post=3304"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/dlhb.art\/da\/wp-json\/wp\/v2\/tags?post=3304"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}