% IMPORTANT: The following is UTF-8 encoded.  This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.

@ARTICLE{Campforts:820925,
      author       = {Campforts, Benjamin and Vanacker, Veerle and Vanderborght,
                      Jan and Baken, Stijn and Smolders, Erik and Govers, Gerard},
      title        = {{S}imulating the mobility of meteoric 10{B}e in the
                      landscape through a coupled soil-hillslope model ({B}e2{D})},
      journal      = {Earth and planetary science letters},
      volume       = {439},
      issn         = {0012-821X},
      address      = {Amsterdam [u.a.]},
      publisher    = {Elsevier},
      reportid     = {FZJ-2016-06189},
      pages        = {143 - 157},
      year         = {2016},
      abstract     = {Meteoric 10Be allows for the quantification of vertical and
                      lateral soil fluxes over long time scales (103–105
                      yr103–105 yr). However, the mobility of meteoric 10Be in
                      the soil system makes a translation of meteoric 10Be
                      inventories into erosion and deposition rates complex. Here,
                      we present a spatially explicit 2D model simulating the
                      behaviour of meteoric 10Be on a hillslope. The model
                      consists of two parts. The first component deals with
                      advective and diffusive mobility of meteoric 10Be within the
                      soil profile, and the second component describes lateral
                      soil and meteoric 10Be fluxes over the hillslope. Soil depth
                      is calculated dynamically, accounting for soil production
                      through weathering as well as downslope fluxes of soil due
                      to creep, water and tillage erosion. Synthetic model
                      simulations show that meteoric 10Be inventories can be
                      related to erosion and deposition across a wide range of
                      geomorphological and pedological settings. Our results also
                      show that meteoric 10Be can be used as a tracer to detect
                      human impact on soil fluxes for soils with a high affinity
                      for meteoric 10Be. However, the quantification of vertical
                      mobility is essential for a correct interpretation of the
                      observed variations in meteoric 10Be profiles and
                      inventories. Application of the Be2D model to natural
                      conditions using data sets from the Southern Piedmont (Bacon
                      et al., 2012) and Appalachian Mountains (Jungers et al.,
                      2009 and West et al., 2013) allows to reliably constrain
                      parameter values. Good agreement between simulated and
                      observed meteoric 10Be concentrations and inventories is
                      obtained with realistic parameter values. Furthermore, our
                      results provide detailed insights into the processes
                      redistributing meteoric 10Be at the soil-hillslope scale.},
      cin          = {IBG-3},
      ddc          = {550},
      cid          = {I:(DE-Juel1)IBG-3-20101118},
      pnm          = {255 - Terrestrial Systems: From Observation to Prediction
                      (POF3-255)},
      pid          = {G:(DE-HGF)POF3-255},
      typ          = {PUB:(DE-HGF)16},
      UT           = {WOS:000371843700015},
      doi          = {10.1016/j.epsl.2016.01.017},
      url          = {https://juser.fz-juelich.de/record/820925},
}