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Plant and soil elemental C:N:P ratios are linked to soil microbial diversity during grassland restoration on the Loess Plateau, China
Yang Y., Liu H., Yang X., Yao H., Deng X., Wang Y., An S., Kuzyakov Y., Chang S.X.
grasslands (1, 5, 10, 15, 25, and 30 years since restoration) on the Loess Plateau. We found that C and N
Fate and transport of urea-N in a rain-fed ridge-furrow crop system with plastic mulch
Guo S., Jiang R., Qu H., Wang Y., Misselbrook T., Gunina A., Kuzyakov Y.
Loess plateau
Transport of late pleistocene loess particles by katabatic winds during the lowstands of the english channel
Lefort J., Monnier J., Danukalova G.
the cementation of stony beaches under a loess blanket. Although the loess cover was later washed out by younger
Afforestation of loess soils: Old and new organic carbon in aggregates and density fractions
Jiang R., Gunina A., Qu D., Kuzyakov Y., Yu Y., Hatano R., Frimpong K.A., Li M.
the dynamics of SOC accumulation after afforestation on the Loess Plateau; ii) to determine SOC contents
Humidity controls soil organic carbon accrual in grassland on the Qinghai–Tibet Plateau
Guan Z.-H., Jia B., Niu Z.-Q., Mou X.-M., Chen J., Li F.-C., Wu Y.-N., Ning S., Yakov K., Li X.G.
of grasslands along an altitudinal gradient from 1286 m on the western Loess Plateau (LP) to 4200 m above sea
Afforestation of loess soils: Old and new organic carbon in aggregates and density fractions
Jiang R., Gunina A., Qu D., Kuzyakov Y., Yu Y., Hatano R., Frimpong K., Li M.
) to investigate the dynamics of SOC accumulation after afforestation on the Loess Plateau; ii) to determine SOC
The δ13C, δ18O and Δ47records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The delta C-13, delta O-18 and Delta(47) records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Lechler A.R., Schauer A.J., Kuzyakov Y., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However
The δ13C, δ18O and Δ 47 records in biogenic, pedogenic and geogenic carbonate types from paleosol-loess sequence and their paleoenvironmental meaning
Zamanian K., Kuzyakov Y., Lechler A.R., Schauer A.J., Huntington K.W.
of carbonate types, including rhizoliths and land-snail shells, present in paleosol-loess sequences. However

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