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Number of items: 11.

Kindler, R; Siemens, J; Kaiser, K; Walmsley, D C; Bernhofers, C; Buchmann, N; Cellier, P; Eugster, W; Gleixner, G; Grünwald, T; Heim, A; Ibrom, A; Jones, S K; Jones, M; Klumpp, K; Kutsch, W; Larsen, K S; Lehuger, S; Loubet, B; McKenzie, R; Moors, E; Osborne, B; Pilegaard, K; Rebmann, C; Saunders, M; Schmidt, M W I; Schrumpf, M; Seyfferth, J; Skiba, U; Soussana, J F; Sutton, M A; Tefs, C; Vowinckel, B; Zeeman, M J; Kaupenhohann, M (2011). Dissolved carbon leaching from soil is a crucial component of the net ecosystem carbon balance. Global Change Biology, 17(2):1167-1185.

Abiven, S; Heim, A; Schmidt, M W I (2011). Lignin content and chemical characteristics in maize and wheat vary between plant organs and growth stages: consequences for assessing lignin dynamics in soil. Plant and Soil, 343(1-2):369-378.

Heim, A; Hofmann, A; Schmidt, M W I (2010). Forest-derived lignin biomarkers in an Australian oxisol decrease substantially after 90 years of pasture. Organic Geochemistry, 41(11):1219-1224.

Gaspert, A; Lüthi, B; Mueller, N J; Bossart, W; Heim, A; Wüthrich, R P; Fehr, T (2009). Subacute allograft failure with dysuria and hematuria in a kidney transplant recipient. American Journal of Kidney Diseases, 54(1):154-158.

Hofmann, A; Heim, A; Christensen, B T; Miltner, A; Gehre, M; Schmidt, M W I (2009). Lignin dynamics in two13C-labelled arable soils during 18 years. European Journal of Soil Science, 60(2):250-257.

Heim, A; Wehrli, L; Eugster, W; Schmidt, M W I (2009). Effects of sampling design on the probability to detect soil carbon stock changes at the Swiss CarboEurope site Lägeren. Geoderma, 149(3-4):347-354.

Heim, A; Moser, N; Blum, H; Schmidt, M W I (2009). How far do experimentally elevated CO2 levels reach into the surrounding?: an example using the13C label of soil organic matter as an archive. Global Change Biology, 15(6):1598-1602.

Hofmann, A; Heim, A; Gioacchini, P; Miltner, A; Gehre, M; Schmidt, M W I (2009). Mineral fertilization did not affect decay of old lignin and SOC in a 13C-labeled arable soil over 36 years. Biogeosciences, 6(7):1139 -1148.

Joos, O; Hagedorn, F; Heim, A; Gilgen, A K; Schmidt, M W I; Siegwolf, R T W; Buchmann, N (2009). Summer drought reduces total and litter-derived soil CO2 effluxes in temperate grassland – clues from a 13C litter addition experiment. Biogeosciences, 6(6):11005 -11034.

Joos, O; Saurer, M; Heim, A; Hagedorn, F; Schmidt, M W I; Siegwolf, R T W (2008). Can we use the CO2 concentrations determined by continuous-flow isotope ratio mass spectrometry from small samples for the Keeling plot approach? Rapid Communications in Mass Spectrometry, 22(24):4029-4034.

Marschner, B; Brodowski, S; Dreves, A; Gleixner, G; Gude, A; Grooles, P M; Hamer, U; Heim, A; Jandl, G; Ji, R; Kaiser, K; Kalbitz, K; Kramer, C; Leinweber, P; Rethemeyer, J; Schäffer, A; Schmidt, M W I; Schwark, L; Wiesenberg, G L B (2008). How relevant is recalcitrance for the stabilization of organic matter in soils? Journal of Plant Nutrition and Soil Science, 171(1):91-110.

This list was generated on Wed Jun 26 18:18:20 2019 CEST.