The effect of landslide on soil organic carbon stock and biochemical properties of soil

Recovery in soil cover and vegetation structure after ancient landslide in mountain fens under Caltho-Alnetum community and response of soil microarthropods (Hexapoda: Collembola) to natural restoration process

“…This result is consistent with van The CCA analysis with interactive stepwise (forward) selection of environmental variables, which indicated that total carbon content in soil was the best predictor of the Collembola community variation, allows us to point out that the postdisturbance heterogeneity in the soil organic matter pool through providing new microhabitats can have a long-term influence on the soil biota distribution pattern. The identified effect of landslide on soil carbon stock and biogeochemical properties in forest soil is consistent with Blońska et al (2018) and Cheng et al (2016) results. The observed changes in the biodiversity and abundance in soil microarthropod communities confirm that landslides play an important role in the maintenance of biodiversity (Geertsma et al 2009).…”

“…During the conducted study, the lowest value of total organic carbon was determined for soils of the second (deluvial) layer in comparison with original (III) and organic (I) layers. According to Blońska et al (2018) and Nicia et al (2018a), the organic carbon and organic matter content play a major role in early stage of formation of soil cover and vegetation.…”

Changes in the physico-chemical properties of topsoil in a landslide-affected area (western part of the Transylvanian Basin, Romania)

“…Thus, this type of study is es sen tial in the construc tion of risk maps for land slides (van Eynde et al, 2017). Or ganic mat ter was used as an in di ca tor of soil qual ity due to the many im por tant in ter ac tions within the soil sys tem (Blonska et al, 2018). Changes in the amount of or ganic soil mat ter, nu tri ents and phys i cal prop er ties have dif fer ent in ten si fica tion de grees within land slides, and strongly in flu ence the processes of soil cover and veg e ta tion res to ra tion (Pickett et al, 1999;Shiels et al, 2006).…”

8. Identifikasi Sifat Kimia Tanah Pada Longsor Aktif Dan Longsor Inaktif (Dormant) Di Desa Margoyoso Kecamatan Salaman Kabupaten Magelang Jawa Tengah

“…Kejadian longsor menyebabkan terjadinya kehilangan tanah, deposisi material sedimen, dan menghasilkan pencampuran material tanah (Eynde, Dondeyne, Isabirye, Decker, & Poesen, 2017). Perubahan yang diakibatkan oleh longsor akan berdampak pada kualitas tanah tersebut (Błońska, Lasota, Piaszczyk, & Wiecheć, 2017). Seringnya kejadian longsor di Sub-DAS Bompon menyebabkan perubahan morfologi dan akan berdampak juga pada kualitas tanah.…”