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Browse By Author Name - Schwen, Andreas
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Weninger, Thomas
,
Bodner, Gernot
,
Kreiselmeier, Janis
,
Chandrasekhar, Parvathy
,
Julich, Stefan
,
Feger, Karl-Heinz
,
Schwärzel, Kai
and
Schwen, Andreas
, (
2018
).
Combination of Measurement Methods for a Wide-Range Description of Hydraulic Soil Properties
.
Water
,
10
(
8
),
1
-
15
739
Weninger, Thomas
,
Kreiselmeier, Janis
,
Chandrasekhar, Parvathy
,
Julich, Stefan
,
Feger, Karl-Heinz
,
Schwärzel, Kai
,
Bodner, Gernot
and
Schwen, Andreas
, (
2019
).
Effects of Tillage Intensity on Pore System and Physical Quality of Silt-Textured Soils Detected by Multiple Methods
.
Soil Research
,
n/a
-
n/a
542
Chandrasekhar, Parvathy
,
Kreiselmeier, Janis
,
Schwen, Andreas
,
Weninger, Thomas
,
Julich, Stefan
,
Feger, Karl-Heinz
and
Schwärzel, Kai
, (
2019
).
Modeling the Evolution of Soil Structural Pore Space in Agricultural Soils Following Tillage
.
Geoderma
,
353
401
-
414
583
Kreiselmeier, Janis
,
Chandrasekhar, Parvathy
,
Weninger, Thomas
,
Schwen, Andreas
,
Julich, Stefan
,
Feger, Karl-Heinz
and
Schwärzel, Kai
, (
2019
).
Quantification of Soil Pore Dynamics During a Winter Wheat Cropping Cycle Under Different Tillage Regimes
.
Soil and Tillage Research
,
192
222
-
232
620
Chandrasekhar, Parvathy
,
Kreiselmeier, Janis
,
Schwen, Andreas
,
Weninger, Thomas
,
Julich, Stefan
,
Feger, Karl-Heinz
and
Schwärzel, Kai
, (
2019
).
SPorDyn: A Python code for modeling the evolution of soil pore size distribution after tillage
.
MethodsX
,
6
2118
-
2126
279
Kreiselmeier, Janis
,
Chandrasekhar, Parvathy
,
Weninger, Thomas
,
Schwen, Andreas
,
Julich, Stefan
,
Feger, Karl-Heinz
and
Schwärzel, Kai
, (
2019
).
Temporal variations of the hydraulic conductivity characteristic under conventional and conservation tillage
.
Geoderma
,
362
1
-
12
271
Chandrasekhar, Parvathy
,
Kreiselmeier, Janis
,
Schwen, Andreas
,
Weninger, Thomas
,
Julich, Stefan
,
Feger, Karl-Heinz
and
Schwärzel, Kai
, (
2018
).
Why We Should Include Soil Structural Dynamics of Agricultural Soils in Hydrological Models
.
Water
,
10
(
12
),
1
-
18
530
