共 19 条
[1]
Pedogenic carbonate carbon isotopic constraints on paleoprecipitation: Evolution of desert in the Pacific Northwest; USA; in response to topographic development of the Cascade Range.[J].Akinori Takeuchi;Michael T. Hren;Shane V. Smith;C. Page Chamberlain;Peter B. Larson.Chemical Geology.2010, 3
[2]
Does long-term center-pivot irrigation increase soil carbon stocks in semi-arid agro-ecosystems?.[J].K. Denef;C.E. Stewart;J. Brenner;K. Paustian.Geoderma.2008, 1
[5]
Land use effects on soil N; P; C and pH persist over 40–80 years of forest growth on agricultural soils.[J]..Forest Ecology and Management.2006, 1
[6]
Irrigation Increases Inorganic Carbon in Agricultural Soils.[J].James A. Entry;R. E. Sojka;Glenn E. Shewmaker.Environmental Management.2004, 1s
[7]
Origin and rate of pedogenic carbonate accumulation in Saskatchewan soils; Canada.[J].A Landi;A.R Mermut;D.W Anderson.Geoderma.2003, 1
[8]
The destruction of paleoclimatic isotopic signals in Pleistocene carbonate soil nodules of Western Australia.[J].David A Budd;Sean M Pack;Marilyn L Fogel.Palaeogeography; Palaeoclimatology; Palaeoecology.2002, 3
[9]
Morphology and isotope heterogeneity of Late Quaternary pedogenic carbonates: Implications for paleosol carbonates as paleoenvironmental proxies.[J]..Palaeogeography; Palaeoclimatology; Palaeoecology.2001, 3
[10]
Quantifying pedogenic carbonate accumulations using stable carbon isotopes.[J].L.C. Nordt;C.T. Hallmark;L.P. Wilding;T.W. Boutton.Geoderma.1998, 1

