2016
DOI: 10.1016/j.still.2016.06.003
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Effects of tillage practices on water consumption characteristics and grain yield of winter wheat under different soil moisture conditions

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Cited by 60 publications
(27 citation statements)
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“…where ρ is the bulk density of the soil of one sample, g/ cm 3 ; m is the dry weight of the soil in the foil sampler, g; and v is the sample volume of the foil sampler, cm 3 .…”
Section: Effects Of Different Tillage Methods On the Bulk Density Of mentioning
confidence: 99%
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“…where ρ is the bulk density of the soil of one sample, g/ cm 3 ; m is the dry weight of the soil in the foil sampler, g; and v is the sample volume of the foil sampler, cm 3 .…”
Section: Effects Of Different Tillage Methods On the Bulk Density Of mentioning
confidence: 99%
“…The water storage in the soil was calculated using Equation 2. The bulk density of the soil at a depth of 0-30 cm was calculated according to the measurements obtained that correlated to each year, and the water content in the soil at a depth of 30-100 cm was calculated according to the average bulk density of 1.46 g/ cm 3 of the soil. The bulk density of the soil at a depth of 30-100 cm changed a little as the depth of tillage was less than 30 cm.…”
Section: Moisture Content Of the Soilmentioning
confidence: 99%
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“…Research is a key driver here because potential new measures of and additional arguments for subsoil management seem to be primarily discussed within the scientific community. Therein, subsoil management is discussed in terms of sequestering carbon (climate change mitigation) (Kell 2012;Alcantara et al 2016;Lorenz and Lal 2005), water conserving tillage (climate change adaptation) (Sang et al 2016), and phosphorous efficiency (resource scarcity) (Ekelöf et al 2015;Zhang et al 2016). Thus, research is now providing more arguments for subsoil management in relation to current societal challenges, thereby potentially creating a meaningful impact.…”
Section: Subsoil Managementmentioning
confidence: 99%
“…Infiltration, one of the most important soil properties, is responsible for water entering the soil; however, it is not easy to measure and predict, as it is highly variable both spatially and temporally [3]. Some major driving forces, such as soil surface crusting due to the high kinetic energy of falling raindrops [4,5]; soil sealing on the surface or at deeper levels (e.g., plough pan [6]); and rill and gully formation, which decreases water contact to the soil surface, decrease infiltration [7], whereas other forces, such as increasing plant growth, surface roughness, and surface coverage [8], increase the volume of infiltration. Ploughing tillage (PT; conventional cultivation system based on annual moldboard ploughing tillage) plays an ambivalent role.…”
Section: Introductionmentioning
confidence: 99%