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University of ZurichFrom line 273, column 37; to line 273, column 138
University of ZurichFrom line 285, column 63; to line 285, column 143
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  140. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/DataCiteXML/zora-eprint-120438.xml" type="application/datacitexml+xml; charset=utf-8" title="DataCite XML (4.4)" />↩
  141. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/Citavi/zora-eprint-120438.xml" type="text/xml" title="Citavi" />↩
  142. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/RIS/zora-eprint-120438.ris" type="text/plain" title="Reference Manager" />↩
  143. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/RDFN3/zora-eprint-120438.n3" type="text/n3" title="RDF+N3" />↩
  144. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/MARC21XML/zora-eprint-120438.xml" type="application/marcxml+xml; charset=utf-8" title="MARC21 XML" />↩
  145. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/CSV/zora-eprint-120438.csv" type="text/csv; charset=utf-8" title="Multiline CSV" />↩
  146. <link rel="alternate" href="https://www.zora.uzh.ch/cgi/export/eprint/120438/ZORACSV/zora-eprint-120438.csv" type="text/csv; charset=utf-8" title="ZORA CSV" />↩
  147. <link rel="http://purl.org/net/sword/discovery/service-document" href="https://www.zora.uzh.ch/sword-app/servicedocument" />↩
  148. <link rel="http://purl.org/net/sword/terms/deposit" href="https://www.zora.uzh.ch/id/contents" />↩
  149. <link rel="search" type="text/html" href="http://www.zora.uzh.ch/cgi/search" />↩
  150. <link rel="search" type="application/opensearchdescription+xml" href="http://www.zora.uzh.ch/cgi/opensearchdescription" title="ZORA" />↩
  151. <script src="https://www.gstatic.com/charts/loader.js"></script><script>↩
  152. // <![CDATA[↩
  153. google.charts.load("current", {packages:["corechart", "geochart"]});↩
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  156. <script>↩
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  159. var eprints_http_cgiroot = "https:\/\/www.zora.uzh.ch\/cgi";↩
  160. var eprints_oai_archive_id = "www.zora.uzh.ch";↩
  161. var eprints_logged_in = false;↩
  162. // ]]></script>↩
  163. <style>.ep_logged_in { display: none }</style>↩
  164. <link rel="stylesheet" type="text/css" href="/style/auto-3.3.16.css" />↩
  165. <script src="/javascript/auto-3.3.16.js"></script>↩
  166. <!--[if lte IE 6]>↩
  167. <link rel="stylesheet" type="text/css" href="/style/ie6.css" />↩
  168. <![endif]-->↩
  169. <meta name="Generator" content="EPrints 3.3.16" />↩
  170. <meta http-equiv="Content-Type" content="text/html; charset=UTF-8" />↩
  171. ↩
  172. <link rel="icon" type="image/png" href="/favicon-32x32.png" sizes="32x32" />↩
  173. ↩
  174. <script src="/javascript/jquery/jquery.min.js"></script>↩
  175. <script src="/zora_zwonull/scripts/main.js"></script>↩
  176. <script src="/zora_zwonull/scripts/menu.js"></script>↩
  177. <script src="/zora_zwonull/scripts/buttons.js"></script>↩
  178. <script src="/zora_zwonull/scripts/workflow.js"></script>↩
  179. <script src="/zora_zwonull/scripts/workflow_icons.js"></script>↩
  180. <script src="/zora_zwonull/scripts/translation.js"></script>↩
  181. <script src="/zora_zwonull/scripts/contributor_citation.js"></script>↩
  182. <script type="text/x-mathjax-config">↩
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  189. });↩
  190. </script>↩
  191. <script src="/javascript/MathJax/MathJax.js?config=TeX-AMS-MML_HTMLorMML"></script>↩
  192. ↩
  193. <!-- Bootstrap -->↩
  194. <meta name="viewport" content="width=device-width, initial-scale=1" />↩
  195. <link href="/zora_zwonull/styles/bootstrap.css" rel="stylesheet" />↩
  196. <script src="/zora_zwonull/scripts/bootstrap.min.js"></script>↩
  197. ↩
  198. <!-- change to local version with little UZH-Changes -->↩
  199. <link href="/zora_zwonull/fonts/font-awesome-4.6.3/css/font-awesome.min.css" rel="stylesheet" /> ↩
  200. <script src="/zora_zwonull/scripts/clipboard.js-master/dist/clipboard.min.js"></script>↩
  201. ↩
  202. <!-- styles -->↩
  203. <link href="/zora_zwonull/styles/main.css" rel="stylesheet" />↩
  204. <link href="/zora_zwonull/styles/search.css" rel="stylesheet" />↩
  205. <link href="/zora_zwonull/styles/recollect_overrides.css" rel="stylesheet" />↩
  206. <link href="/zora_zwonull/styles/zora_zwonull.css" rel="stylesheet" />↩
  207. <link href="/zora_zwonull/styles/summary.css" rel="stylesheet" />↩
  208. <link href="/zora_zwonull/styles/front_page.css" rel="stylesheet" />↩
  209. ↩
  210. <!-- finally the theme color -->↩
  211. <meta name="theme-color" content="#3570b1" />↩
  212. ↩
  213. <!-- Piwik/Matomo -->↩
  214. <script>↩
  215. var _paq = _paq || [];↩
  216. // tracker methods like "setCustomDimension" should be called before "trackPageView"↩
  217. _paq.push(['trackPageView']);↩
  218. _paq.push(['enableLinkTracking']);↩
  219. (function() {↩
  220. var u="//webstats.uzh.ch/";↩
  221. _paq.push(['setTrackerUrl', u+'piwik.php']);↩
  222. _paq.push(['setSiteId', '254']);↩
  223. var d=document, g=d.createElement('script'), s=d.getElementsByTagName('script')[0];↩
  224. g.type='text/javascript'; g.async=true; g.defer=true; g.src=u+'piwik.js'; s.parentNode.insertBefore(g,s);↩
  225. })();↩
  226. </script>↩
  227. <!-- End Piwik/Matomo Code -->↩
  228. </head>↩
  229. ↩
  230. <body>↩
  231. <!-- body: header, nav, main, footer -->↩
  232. <header>↩
  233. <h2 class="visually-hidden"> Header </h2>↩
  234. ↩
  235. </header>↩
  236. ↩
  237. ↩
  238. <nav aria-describedby="skiplinknav" class="skiplinks js-skiplinks" id="skiplinks">↩
  239. <h3 class="visually-hidden" id="skiplinknav">Quicknavigation</h3>↩
  240. <ul>↩
  241. <li>↩
  242. <a accesskey="0" href="/" title="[ALT + 0]">Home</a>↩
  243. </li>↩
  244. <li>↩
  245. <a accesskey="1" href="#topnav" title="[ALT + 1]">Navigation</a>↩
  246. </li>↩
  247. <li>↩
  248. <a accesskey="2" href="#page" title="[ALT + 2]">Content</a>↩
  249. </li>↩
  250. <li>↩
  251. <a accesskey="3" href="mailto:oai@hbz.uzh.ch" title="[ALT + 3]">Contact</a>↩
  252. </li>↩
  253. <li>↩
  254. <a accesskey="5" href="#repo_search" title="[ALT + 5]">Search</a>↩
  255. </li>↩
  256. </ul>↩
  257. </nav>↩
  258. ↩
  259. ↩
  260. <nav>↩
  261. <h3 class="visually-hidden"> Navigation </h3>↩
  262. <div id="uzh-navbar" class="navbar navbar-default" role="navigation">↩
  263. <div class="container-fluid">↩
  264. <!-- Brand and toggle get grouped for better mobile display -->↩
  265. <div class="navbar-header">↩
  266. <button type="button" class="navbar-toggle" data-toggle="collapse" data-target="#lowernav">↩
  267. <span class="sr-only">Toggle navigation</span>↩
  268. <span class="icon-bar"></span>↩
  269. <span class="icon-bar"></span>↩
  270. <span class="icon-bar"></span>↩
  271. </button>↩
  272. <div class="visible-xs" id="xs_header_icons">↩
  273. <a href="http://www.uzh.ch"><img src="/images/uzh_logo_en.jpg" alt="University of Zurich" data-pixelate="true" data-value="0.1" /></a>↩
  274. <a href="https://www.zora.uzh.ch">↩
  275. <span class="fa fa-home fa-lg"></span>↩
  276. <span class="fa-zora fa-lg">ZORA</span>↩
  277. </a>↩
  278. </div>↩
  279. </div>↩
  280. <!-- Collect the nav links, forms, and other content for toggling -->↩
  281. <!-- 1. Navi: Top Navi with external links -->↩
  282. <nav class="col-md-2 col-sm-2 col-xs-12 hidden-print">↩
  283. <div class="hidden-xs"> ↩
  284. <ul class="nav nav-pills nav-stacked">↩
  285. <li> <a href="http://www.uzh.ch" class="uzh_logo"><img class="uzh_logo" src="/images/uzh_logo_en.jpg" alt="University of Zurich" /></a></li>↩
  286. </ul>↩
  287. </div>↩
  288. </nav>↩
  289. ↩
  290. <nav class="visible-lg col-lg-offset-2 collapse navbar-collapse" id="topnav">↩
  291. <ul class="nav navbar-nav navbar-left">↩
  292. <li><a href="https://www.zora.uzh.ch" title="ZORA Homepage">↩
  293. <span class="fa fa-home fa-lg" aria-hidden="true">↩
  294. </span> ZORA↩
  295. <span class="sr-only">↩
  296. Homepage↩
  297. </span>↩
  298. </a></li>↩
  299. <li> <a href="https://ub.uzh.ch/de/wissenschaftlich-arbeiten/publizieren/Publizieren-auf-UZH-Plattformen/publizierter-inhalt-auf-ZORA">About ZORA</a> </li>↩
  300. <li> <a href="https://ub.uzh.ch/de/ueber-die-ub/ub_organisation/ub_mitarbeitende.html#Open_science_services"><abbr title="Team Open Access at Main Library University of Zurich">OA-Team</abbr></a> </li>↩
  301. <li> <a href="https://www.zora.uzh.ch/cgi/stats/report">Statistics</a> </li>↩
  302. <li id="lia_login"><a href="https://www.zora.uzh.ch/cgi/users/home">Login</a></li>↩
  303. ↩
  304. <li><a href="/cgi/set_lang?lang=de&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_first" title="Link zur deutschen Sprachversion">DE</a></li><li><a href="/cgi/set_lang?lang=en&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_next" title="Visit the english page">EN</a></li>↩
  305. </ul>↩
  306. <ul class="visible-xs nav navbar-nav navbar-left">↩
  307. <li> <a href="/">ZORA</a></li>↩
  308. <li><a href="/cgi/set_lang?lang=de&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_first" title="Link zur deutschen Sprachversion">DE</a></li><li><a href="/cgi/set_lang?lang=en&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_next" title="Visit the english page">EN</a></li>↩
  309. </ul>↩
  310. <ul class="visible-md visible-lg nav navbar-nav navbar-right">↩
  311. ↩
  312. <!-- next ZORA-897 oa@ub.uzh.ch -->↩
  313. <li><a href="mailto:oai@hbz.uzh.ch" title="Contact Open Access Team via Email">↩
  314. <span class="fa fa-envelope-square fa-lg" aria-hidden="true">↩
  315. </span> oai@hbz.uzh.ch↩
  316. <span class="sr-only">↩
  317. Contact Open Access Team via Email↩
  318. </span>↩
  319. </a></li>↩
  320. <!-- ZORA-897 2021/12/22/jw - temp. out of service until new links are born in 2022↩
  321. <li><a href="https://www.facebook.com/uzh.hauptbibliothek" title="Visit the Facebook page of Main Library at UZH">↩
  322. <span class="fa fa-facebook-square fa-lg" aria-hidden="true">↩
  323. </span>↩
  324. <span class="sr-only">↩
  325. Visit the Facebook page of Main Library at UZH↩
  326. </span>↩
  327. </a></li>↩
  328. <li><a href="https://www.youtube.com/user/uzhhbz" title="Visit the YouTube channel of Main Library at UZH">↩
  329. <span class="fa fa-youtube-square fa-lg" aria-hidden="true">↩
  330. </span>↩
  331. <span class="sr-only">↩
  332. Visit the YouTube channel of Main Library at UZH↩
  333. </span>↩
  334. </a></li>↩
  335. <li><a href="https://twitter.com/uzh_hbz" title="Visit the Twitter channel of Main Library at UZH">↩
  336. <span class="fa fa-twitter-square fa-lg" aria-hidden="true">↩
  337. </span>↩
  338. <span class="sr-only">↩
  339. Visit the Twitter channel of Main Library at UZH↩
  340. </span>↩
  341. </a></li>↩
  342. -->↩
  343. ↩
  344. </ul>↩
  345. </nav> <!-- /.navbar-collapse #topnav-->↩
  346. </div> <!-- /.container-fluid -->↩
  347. </div> <!-- /#uzh-navbar -->↩
  348. ↩
  349. <!-- 2. Navi: Admin if logged in, not mobile -->↩
  350. <nav class="visible-lg visible-md" id="adminnav">↩
  351. ↩
  352. </nav>↩
  353. ↩
  354. <!-- 3. Navi: ZORA Browsing -->↩
  355. <nav class="collapse navbar-collapse oai_logo col-lg-offset-2 col-md-offset-2 col-sm-offset-2 col-xs-offset-1" id="lowernav"> ↩
  356. <span class="sr-only">Browse by:</span>↩
  357. <ul class="nav navbar-nav hidden-print"> ↩
  358. <li>↩
  359. <a href="https://www.zora.uzh.ch/view/yearnew/">↩
  360. Year↩
  361. </a>↩
  362. </li>↩
  363. <li>↩
  364. <a href="https://www.zora.uzh.ch/creators_editors.html">↩
  365. Creators &amp; Editors↩
  366. </a>↩
  367. </li>↩
  368. <li>↩
  369. <a href="https://www.zora.uzh.ch/view/subjectsnew/">↩
  370. Communities &amp; Collections↩
  371. </a>↩
  372. </li>↩
  373. <li>↩
  374. <a href="https://www.zora.uzh.ch/view/dewey/">↩
  375. DDC↩
  376. </a>↩
  377. </li>↩
  378. <li>↩
  379. <a href="https://www.zora.uzh.ch/view/scopussubjects/">↩
  380. Scopus Subject Areas↩
  381. </a>↩
  382. </li>↩
  383. </ul>↩
  384. <ul class="nav navbar-nav hidden-lg hidden-md hidden-sm">↩
  385. <li> <a href="https://www.zora.uzh.ch/cgi/stats/report">Statistics</a> </li>↩
  386. <li><a href="/cgi/set_lang?lang=de&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_first" title="Link zur deutschen Sprachversion">DE</a></li><li><a href="/cgi/set_lang?lang=en&amp;referrer=https%3A%2F%2Fwww.zora.uzh.ch%2Fid%2Feprint%2F120438%2F" class="lang_next" title="Visit the english page">EN</a></li>↩
  387. ↩
  388. </ul>↩
  389. </nav> <!-- /#lowernav -->↩
  390. ↩
  391. <!-- search bar -->↩
  392. ↩
  393. <div id="repo_search" class="container-fluid hidden-print">↩
  394. <section>↩
  395. <script>↩
  396. // local settings, goto react for initial settings↩
  397. var label_searchbox_placeholder = "Search in metadata and fulltext";↩
  398. var label_searchbutton = "Search";↩
  399. var label_reset_all = "Clear all";↩
  400. var label_advanced_search = "Advanced Search";↩
  401. var label_help = "Help";↩
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  404. ↩
  405. ↩
  406. <link rel="manifest" href="/faceted-search/manifest.json"/>↩
  407. <noscript>You need to enable JavaScript to run this app.</noscript>↩
  408. ↩
  409. <div id="root"></div>↩
  410. ↩
  411. <link href="/faceted-search/static/css/2.238ba706.chunk.css" rel="stylesheet">↩
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  413. <script src="/faceted-search/static/js/2.a43d7600.chunk.js"></script><script src="/faceted-search/static/js/main.4a34f682.chunk.js"></script>↩
  414. </section>↩
  415. <!-- new position search more start -->↩
  416. <div class="col-md-offset-0 col-lg-11 col-md-11 col-sm-10 hidden-xs">↩
  417. <ul id="search_more">↩
  418. <li> <a href="https://www.zora.uzh.ch/cgi/search/advanced">Advanced Search</a></li>↩
  419. <li> <a href="https://www.zora.uzh.ch/help">Help</a></li>↩
  420. </ul>↩
  421. </div>↩
  422. </div>↩
  423. ↩
  424. ↩
  425. </nav>↩
  426. ↩
  427. <main id="page" class="col-lg-12 col-md-12 col-sm-12 col-xs-12">↩
  428. ↩
  429. <div class="shadow container-fluid">↩
  430. <p class="visible-print-block">↩
  431. <img src="/images/uzh_logo_en.jpg" alt="UZH-Logo" />↩
  432. </p>↩
  433. <div class="col-lg-12 col-md-12 col-sm-12 col-xs-12" id="main_title">↩
  434. <span class="zora_maintenance_xs hidden-print visible-xs"> <a href="/zora_maintenance.html">Maintenance Infos</a></span>↩
  435. <h1> ↩
  436. ↩
  437. Mass fluxes and clay mineral formation in soils developed on slope deposits of the Kowarski Grzbiet (Karkonosze Mountains, Czech Republic/Poland)↩
  438. ↩
  439. </h1>↩
  440. <div class="hidden-print hidden-xs"> ↩
  441. <!-- maintenance message -->↩
  442. ↩
  443. ↩
  444. ↩
  445. ↩
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  448. <div class="ep_summary_content"><div class="ep_summary_content_left"></div><div class="ep_summary_content_right"></div><div class="ep_summary_content_top"></div><div class="ep_summary_content_main"><script src="/javascript/jquery/jquery.min.js"></script><script src="/zora_zwonull/scripts/read_less_more/readmore.js"></script><div class="panel-body visible-xs" style="padding:0px;"></div><br /><div id="e2_column" class="col-lg-12 col-md-12 col-sm-12 col-xs-12 summary-widget"><div class="col-md-8 e2_column_left"><div id="citation_box" class="summary-citation"><p id="citation_text" class="well-dl citation_cb_p" lang="en"><a href="javascript:contributorCitation( 'Waroszewski, Jaroslaw' );" title="Show all publications from &quot;Waroszewski, Jaroslaw&quot;">Waroszewski, Jaroslaw</a>; <a href="javascript:contributorCitation( 'Egli, Markus' );" title="Show all publications from &quot;Egli, Markus&quot;">Egli, Markus</a>; <a href="javascript:contributorCitation( 'Kabala, Cezary' );" title="Show all publications from &quot;Kabala, Cezary&quot;">Kabala, Cezary</a>; <a href="javascript:contributorCitation( 'Kierczak, Jakub' );" title="Show all publications from &quot;Kierczak, Jakub&quot;">Kierczak, Jakub</a>; <a href="javascript:contributorCitation( 'Brandová, Dagmar' );" title="Show all publications from &quot;Brandová, Dagmar&quot;">Brandová, Dagmar</a> (2016). <em>Mass fluxes and clay mineral formation in soils developed on slope deposits of the Kowarski Grzbiet (Karkonosze Mountains, Czech Republic/Poland).</em> Geoderma, 264:363-378.</p><button id="citation_text_copy_button" class="btn-clipboard hidden-xs hidden-print" data-clipboard-target="#citation_text">Copy</button><script src="/zora_zwonull/scripts/clipboard.js-master/zora_clipboard.js"></script></div><article class="hidden-print"><h2 style="margin-left:0px;">Abstract</h2><p id="more_less" lang="en">Weathering, mineral formation, and transformation processes along slopes are complex. In cool mountainous regions, undisturbed soil development with a strong vertical leaching element may abruptly change as a result of erosion, accumulation, lateral water fluxes and aeolian input. We investigated soils in the eastern Karkonosze Mountains that have developed on silicatic slope deposits. To date, illite, vermiculite and chlorite are the minerals that have been detected in the clay fraction. Although the climate and parent material should be favourable for the formation of smectites, expandable phases were not verified so far. We investigated if expandable phases could be detected and how they related to elemental fluxes along a short slope sequence (1142–1268 m a.s.l. on the border between the Czech Republic and Poland). Mass balance calculations indicated intensive mineral weathering together with a significant leaching of Mg, Al, Ca and Mn on the shoulder and foot slope positions. In the middle zone, which has a concave or undulating surface shape, however, the mass balances of several elements (Na, K, Al, P) revealed a less pronounced leaching (corresponding to a lower degree of podsolization) and in some cases even accumulation. At all sites, mass balance calculations and detected soil minerals (e.g. the increase in illite towards the surface together with an increase in Al and K) indicate some aeolian input. Kaolinite was detected in all soil horizons. Its concentration slightly increased towards the soil surface. Together with the pronounced leaching of Ca, part of kaolinite originates from plagioclase weathering. Besides being a weathering product of primary minerals, part of the kaolinite is inherited from the parent material and probably is also due to aeolian input. In all soils, illite was being transformed into vermiculite and smectites (through regularly-interstratified illite-smectite phases). In addition, the content of chloritic components which increases with depth indicated their concurrent weathering and transformation into smectites. Amphibole also may have acted as a source of smectites. Not all smectite is being actively formed in the soil. Most likely due to slope processes (cover beds) that affected even the subsoil, some smectite has been transferred along the slope. Part of the smectite also seems to derive from the parent material. Active formation of expandable clay minerals is related to convex and planar landscape forms. This relationship suggests intense element leaching, inheritance from the parent material and cover bed mixing processes have contributed to the presence of smectite. Along the slope, zones with predominant vertical transport (shoulder, foot slopes) may repeatedly be interchanged with zones dominated by lateral transport (undulating slope, concave forms).</p></article><div class="visible-print-block"><h2>Abstract</h2><p lang="en">Weathering, mineral formation, and transformation processes along slopes are complex. In cool mountainous regions, undisturbed soil development with a strong vertical leaching element may abruptly change as a result of erosion, accumulation, lateral water fluxes and aeolian input. We investigated soils in the eastern Karkonosze Mountains that have developed on silicatic slope deposits. To date, illite, vermiculite and chlorite are the minerals that have been detected in the clay fraction. Although the climate and parent material should be favourable for the formation of smectites, expandable phases were not verified so far. We investigated if expandable phases could be detected and how they related to elemental fluxes along a short slope sequence (1142–1268 m a.s.l. on the border between the Czech Republic and Poland). Mass balance calculations indicated intensive mineral weathering together with a significant leaching of Mg, Al, Ca and Mn on the shoulder and foot slope positions. In the middle zone, which has a concave or undulating surface shape, however, the mass balances of several elements (Na, K, Al, P) revealed a less pronounced leaching (corresponding to a lower degree of podsolization) and in some cases even accumulation. At all sites, mass balance calculations and detected soil minerals (e.g. the increase in illite towards the surface together with an increase in Al and K) indicate some aeolian input. Kaolinite was detected in all soil horizons. Its concentration slightly increased towards the soil surface. Together with the pronounced leaching of Ca, part of kaolinite originates from plagioclase weathering. Besides being a weathering product of primary minerals, part of the kaolinite is inherited from the parent material and probably is also due to aeolian input. In all soils, illite was being transformed into vermiculite and smectites (through regularly-interstratified illite-smectite phases). In addition, the content of chloritic components which increases with depth indicated their concurrent weathering and transformation into smectites. Amphibole also may have acted as a source of smectites. Not all smectite is being actively formed in the soil. Most likely due to slope processes (cover beds) that affected even the subsoil, some smectite has been transferred along the slope. Part of the smectite also seems to derive from the parent material. Active formation of expandable clay minerals is related to convex and planar landscape forms. This relationship suggests intense element leaching, inheritance from the parent material and cover bed mixing processes have contributed to the presence of smectite. Along the slope, zones with predominant vertical transport (shoulder, foot slopes) may repeatedly be interchanged with zones dominated by lateral transport (undulating slope, concave forms).</p></div> ↩
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<h1> Mass fluxes and clay mineral formation in soils developed on slope deposits of the Kowarski Grzbiet (Karkonosze Mountains, Czech Republic/Poland)

<h2> Abstract

<h2> Abstract

<h2> Statistics

<h3> Citations

<h3> Altmetrics

<h3> Downloads

<h2> Additional indexing

<h2> Download

<h2> Green Open Access

<h2> Article Networks

<h3> TrendTerms

<h3> Authors, Affiliations, Collaborations

<h3> Similar Publications

<h2> Footer

<h3> Contact

<h3> Data Policies

<h3> OAI 2.0

<h3> OpenAIRE

<h3> ORCID

<h3> EPrints Software

<h3> Third Party Data

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  2. Mass fluxes and clay mineral formation in soils developed on slope deposits of the Kowarski Grzbiet (Karkonosze Mountains, Czech Republic/Poland)
    1. Abstract
    2. Abstract
    3. Statistics
      1. Citations
      2. Altmetrics
      3. Downloads
    4. Additional indexing
    5. Download
    6. Green Open Access
    7. [nav element with no heading]
    8. Article Networks
      1. TrendTerms
      2. Authors, Affiliations, Collaborations
      3. Similar Publications
    9. Footer
      1. Contact
      2. Data Policies
      3. OAI 2.0
      4. OpenAIRE
      5. ORCID
      6. EPrints Software
      7. Third Party Data

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