Detecting small-scale spatial heterogeneity and temporal dynamics of soil organic carbon (SOC) stocks: a comparison between automatic chamber-derived C budgets and repeated soil inventories

被引:23
作者
Hoffmann, Mathias [1 ]
Jurisch, Nicole [2 ]
Alba, Juana Garcia [1 ]
Borraz, Elisa Albiac [1 ]
Schmidt, Marten [2 ]
Huth, Vytas [2 ]
Rogasik, Helmut [1 ]
Rieckh, Helene [1 ]
Verch, Gernot [3 ]
Sommer, Michael [1 ,4 ]
Augustin, Juergen [2 ]
机构
[1] Leibniz Ctr Agr Landscape Res ZALF, Inst Soil Landscape Res, Eberswalder Str 84, D-15374 Muncheberg, Germany
[2] Leibniz Ctr Agr Landscape Res ZALF, Inst Landscape Biogeochem, Eberswalder Str 84, D-15374 Muncheberg, Germany
[3] Leibniz Ctr Agr Landscape Res ZALF, Res Stn Dedelow, Eberswalder Str 84, D-15374 Muncheberg, Germany
[4] Univ Potsdam, Inst Earth & Environm Sci, Karl Liebknecht Str 24-25, D-14476 Potsdam, Germany
关键词
NET ECOSYSTEM EXCHANGE; NORTH CENTRAL REGION; NO-TILL ECOSYSTEM; EDDY COVARIANCE; CO2; FLUXES; DIOXIDE EXCHANGE; GAS-EXCHANGE; AGRICULTURAL LANDSCAPES; MONITORING NETWORKS; CROP ROTATIONS;
D O I
10.5194/bg-14-1003-2017
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
Carbon (C) sequestration in soils plays a key role in the global C cycle. It is therefore crucial to adequately monitor dynamics in soil organic carbon (Delta SOC) stocks when aiming to reveal underlying processes and potential drivers. However, small-scale spatial (10-30 m) and temporal changes in SOC stocks, particularly pronounced in arable lands, are hard to assess. The main reasons for this are limitations of the well-established methods. On the one hand, repeated soil inventories, often used in long-term field trials, reveal spatial patterns and trends in Delta SOC but require a longer observation period and a sufficient number of repetitions. On the other hand, eddy covariance measurements of C fluxes towards a complete C budget of the soil-plant-atmosphere system may help to obtain temporal Delta SOC patterns but lack small-scale spatial resolution. To overcome these limitations, this study presents a reliable method to detect both short-term temporal dynamics as well as small-scale spatial differences of Delta SOC using measurements of the net ecosystem carbon balance (NECB) as a proxy. To estimate the NECB, a combination of automatic chamber (AC) measurements of CO2 exchange and empirically modeled aboveground biomass development (NPPshoot / were used. To verify our method, results were compared with Delta SOC observed by soil resampling. Soil resampling and AC measurements were performed from 2010 to 2014 at a colluvial depression located in the hummocky ground moraine landscape of northeastern Germany. The measurement site is characterized by a variable groundwater level (GWL) and pronounced small-scale spatial heterogeneity regarding SOC and nitrogen (Nt) stocks. Tendencies and magnitude of Delta SOC values derived by AC measurements and repeated soil inventories corresponded well. The period of maximum plant growth was identified as being most important for the development of spatial differences in annual Delta SOC. Hence, we were able to confirm that AC-based C budgets are able to reveal small-scale spatial differences and short-term temporal dynamics of Delta SOC.
引用
收藏
页码:1003 / 1019
页数:17
相关论文
共 77 条
  • [1] Changes in CO2 emissions after crop conversion from continuous maize to alfalfa
    Alberti, Giorgio
    Delle Vedove, Gemini
    Zuliani, Michel
    Peressotti, Alessandro
    Castaldi, Simona
    Zerbi, Giuseppe
    [J]. AGRICULTURE ECOSYSTEMS & ENVIRONMENT, 2010, 136 (1-2) : 139 - 147
  • [2] Assessing the eddy covariance technique for evaluating carbon dioxide exchange rates of ecosystems: past, present and future
    Baldocchi, DD
    [J]. GLOBAL CHANGE BIOLOGY, 2003, 9 (04) : 479 - 492
  • [3] Batjes NH, 2015, SCOPE SER, V71, P188, DOI 10.1079/9781780645322.0188
  • [4] The significance of the erosion-induced terrestrial carbon sink
    Berhe, Asmeret Asefaw
    Harte, John
    Harden, Jennifer W.
    Torn, Margaret S.
    [J]. BIOSCIENCE, 2007, 57 (04) : 337 - 346
  • [5] Erosion, deposition, and the persistence of soil organic matter: mechanistic considerations and problems with terminology
    Berhe, Asmeret Asefaw
    Kleber, Markus
    [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 2013, 38 (08) : 908 - 912
  • [6] Bolinder MA, 2012, CAN J SOIL SCI, V92, P821, DOI [10.4141/CJSS2012-036, 10.4141/cjss2012-036]
  • [7] CO2 fluxes in adjacent new and permanent temperate grasslands
    Byrne, KA
    Kiely, G
    Leahy, P
    [J]. AGRICULTURAL AND FOREST METEOROLOGY, 2005, 135 (1-4) : 82 - 92
  • [8] How has soil carbon stock changed over recent decades?
    Chen, Leiyi
    Smith, Pete
    Yang, Yuanhe
    [J]. GLOBAL CHANGE BIOLOGY, 2015, 21 (09) : 3197 - 3199
  • [9] Measuring and monitoring soil organic carbon stocks in agricultural lands for climate mitigation
    Conant, Richard T.
    Ogle, Stephen M.
    Paul, Eldor A.
    Paustian, Keith
    [J]. FRONTIERS IN ECOLOGY AND THE ENVIRONMENT, 2011, 9 (03) : 169 - 173
  • [10] Culman SW, 2013, AGRON J, V105, P493, DOI [10.2134/agronj2012.0382, 10.2134/agronj2012.0382er, 10.2134/agronj2012.0273]