Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - New Zealand Journal …, 2017 - Taylor & Francis
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

[PDF][PDF] Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - 2016 - researchgate.net
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

[引用][C] Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann… - … Zealand Journal of …, 2017 - ui.adsabs.harvard.edu
Complexity of clay mineral formation during 120,000 years of soil development along the Franz
Josef chronosequence, New Zealand - NASA/ADS Now on home page ads icon ads Enable …

Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - New Zealand Journal …, 2017 - inis.iaea.org
[en] Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - 2017 - researcharchive.lincoln.ac.nz
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand.

J Dietel, R Dohrmann, G Guggenberger… - 2017 - cabidigitallibrary.org
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - … Zealand Journal of …, 2017 - ingentaconnect.com
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

[PDF][PDF] Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - … OF GEOLOGY AND …, 2017 - researchgate.net
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …

Complexity of clay mineral formation during 120,000 years of soil development along the Franz Josef chronosequence, New Zealand

J Dietel, R Dohrmann, G Guggenberger… - 2017 - researcharchive.lincoln.ac.nz
Weathering of primary silicates to secondary clay minerals over time affects multiple soil
functions such as the accumulation of organic matter and nutrient cations. However, the …