SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:lup.lub.lu.se:4a57f27f-01e9-4bc9-aed1-63cfa753de3d"
 

Search: onr:"swepub:oai:lup.lub.lu.se:4a57f27f-01e9-4bc9-aed1-63cfa753de3d" > Tendency of soil er...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Tendency of soil erosion dynamics by coupling radioisotopes and RUSLE model on the Southeastern Tibetan Plateau in response to climate warming and human activity

Chen, Peng (author)
Hohai University
Czymzik, Markus (author)
Leibniz Institute for Baltic Sea Research Wardemünde
Yu, Zhongbo (author)
Hohai University
show more...
Aldahan, Ala (author)
United Arab Emirates University
Wang, Jinguo (author)
Hohai University
Yi, Peng (author)
Hohai University
Hou, Xiaolin (author)
Technical University of Denmark
Guo, Shouyan (author)
Hohai University
Zheng, Minjie (author)
Lund University,Lunds universitet,MERGE: ModElling the Regional and Global Earth system,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,Kvartärgeologi,Geologiska institutionen,Centre for Environmental and Climate Science (CEC),Faculty of Science,Quaternary Sciences,Department of Geology
show less...
 (creator_code:org_t)
Elsevier BV, 2023
2023
English.
In: Catena. - : Elsevier BV. - 0341-8162. ; 223
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • Soil erosion has created landscape problems in many parts of the world and in particular in cold regions where the sensitive permafrost conditions have changed due to climate warming. Such a case occurred in the Tibetan Plateau (TP), which has been strongly affected by global warming and human activities. Monitoring technologies, like remote sensing and field surveys were used to explore soil erosion rates in the TP, but they were limited by the resolution and meteorological disturbance factors or the spatial and time scales. Here, we present for the first time 210Pbex (excess lead-210) and 137Cs (caesium-137) data of soils from the southeastern TP (SETP) covering an area of 640,000 km2. In the permafrost-dominant areas, the results show mean soil-erosion rates in the last 56–100 years that were relatively higher (1891 t·km−2·a-1) based on 210Pbex than those based on 137Cs (1623 t·km−2·a-1). Modelling results from the Revised Universal Soil Loss Equation (RUSLE) indicate relatively high mean soil erosion rates of 4363 and 4394 t·km−2·a-1 using a period covering the last 40 or 10 years respectively. Our data suggest accelerating erosion rates on the SETP that are linked to permafrost degradation, and glacier and snow melting due to accelerating global climate warming. The increase in ground surface temperature of ∼2 °C in the last four decades has further shifted the regional hydrology, affecting the degeneration of vegetation cover and a further increase in soil-erosion rates. However, our radionuclides data also expose low erosion rates in the seasonally frozen ground at some sampling sites which indicates the complex nature of erosion trends in cold regions that require careful adaptation of soil management.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Naturgeografi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Physical Geography (hsv//eng)

Keyword

Pb and Cs
Climate warming and human activity
RUSLE
Soil erosion
Southeastern Tibetan Plateau

Publication and Content Type

art (subject category)
ref (subject category)

Find in a library

  • Catena (Search for host publication in LIBRIS)

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

Search outside SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Close

Copy and save the link in order to return to this view