Soil resistance under grazed intermediate wheatgrass

2008 ◽  
Vol 88 (5) ◽  
pp. 833-836 ◽  
Author(s):  
M A Liebig ◽  
J R Hendrickson ◽  
J D Berdahl ◽  
J F Karn
Keyword(s):  
Great Plains ◽  
Cropping System ◽  
Soil Bulk Density ◽  
Northern Great Plains ◽  
System Management ◽  
Thinopyrum Intermedium ◽  
Soil Organic C ◽  
Soil Functions ◽  
Organic C ◽  
Intermediate Wheatgrass

Intermediate wheatgrass [Thinopyrum intermedium (Host) Barkw. & D.R. Dewey subsp. intermedium] is a productive, high-quality perennial forage that lacks persistence under grazing. A study was conducted to evaluate the effects of three grazing times on soil bulk density, soil pH, and soil organic C under intermediate wheatgrass. Treatment effects on the three soil attributes were negligible, implying grazing time did not negatively impact intermediate wheatgrass beyond a threshold whereby critical soil functions were impaired. Findings from this study are important in the context of sustainable forage and cropping system management, where maintaining or improving critical soil functions are essential for enhancing agroecosystem sustainability. Key words: Seeded perennial forages, Northern Great Plains, soil organic C

An economic comparison of alternative and traditional cropping systems in the northern Great Plains, USA

2006 ◽  
Vol 21 (1) ◽  
pp. 68-73 ◽  
Author(s):  
Eric A. DeVuyst ◽  
Thomas Foissey ◽  
George O. Kegode
Keyword(s):  
North Dakota ◽  
Great Plains ◽  
Cropping Systems ◽  
Cropping System ◽  
Conventional Tillage ◽  
Northern Great Plains ◽  
Yield Data ◽  
Government Program ◽  
Current Production ◽  
Commodity Programs

AbstractCurrent production practices in the Red River Valley of North Dakota and Minnesota involve use of extensive tillage and/or herbicides to control weeds. Given the erosion potential, environmental concerns associated with herbicides, and herbicide-resistant weeds, alternative cropping systems that mitigate these problems need to be assessed economically. Furthermore, the role that government commodity programs play in the adoption of more ecologically friendly cropping systems needs to be determined. We evaluated 8 years of yield data (1994–2001) from field plots near Fargo, North Dakota, to compare the economics of two alternative cropping systems, reduced-input (RI) and no-till (NT), to a conventional tillage (CT) cropping system. The RI system relies on a more diverse rotation of soybean (SB), spring wheat (SW), sweet clover (SC) and rye, and uses fewer herbicide and fertilizer inputs than CT or NT. Both NT and CT systems rotate SB and SW. We found that CT returns averaged over $47 ha−1more than NT during the study period. Because SC yield data were not available, the economic competitiveness of RI was calculated using break-even yields and returns for SC. Historical SC yields in Cass County, North Dakota were not statistically different from the break-even yields. However, when government program payments were considered, break-even returns for SC increased by about $15 and $18 ha−1and break-even yields by 0.44 and 0.52 MT ha−1for RI to compare with NT and CT, respectively. These results indicate that CT management offers greater economic return than either RI or NT and that government program payments impede adoption of more environmentally friendly cropping systems in the northern Great Plains.

scholarly journals Crop Diversity Effects on Near-Surface Soil Condition under Dryland Agriculture

2014 ◽  
Vol 2014 ◽  
pp. 1-7 ◽  
Author(s):  
Mark A. Liebig ◽  
David W. Archer ◽  
Don L. Tanaka
Keyword(s):  
Agricultural Land ◽  
Cropping Systems ◽  
Cropping System ◽  
Soil Condition ◽  
Crop Diversity ◽  
Northern Great Plains ◽  
Total N ◽  
Near Surface ◽  
Organic C ◽  
South Central

Unprecedented changes in agricultural land use throughout the northern Great Plains of North America have highlighted the need to better understand the role of crop diversity to affect ecosystem services derived from soil. This study sought to determine the effect of four no-till cropping systems differing in rotation length and crop diversity on near-surface (0 to 10 cm) soil properties. Cropping system treatments included small grain-fallow (SG-F) and three continuously cropped rotations (3 yr, 5 yr, and Dynamic) located in south-central North Dakota, USA. Soil pH was lower in the 3 yr rotation (5.17) compared to the Dynamic (5.51) and SG-F (5.55) rotations(P≤0.05). Among cropping system treatments, 5 yr and Dynamic rotations possessed significantly greater soil organic C (SOC) and total N (mean = 26.3 Mg C ha−1, 2.5 Mg N ha−1) compared to the 3 yr (22.7 Mg C ha−1, 2.2 Mg N ha−1) and SG-F (19.9 Mg C ha−1, 2.0 Mg N ha−1) rotations(P≤0.05). Comparison of SOC measured in this study to baseline values at the research site prior to the establishment of treatments revealed only the 5 yr and Dynamic rotations increased SOC over time. The results of this study suggest that a diverse portfolio of crops is necessary to minimize soil acidification and increase SOC.

Soil carbon sequestration and density distribution in a Vertosol under different farming practices

Soil Research ◽  
2004 ◽  
Vol 42 (8) ◽  
pp. 875 ◽  
Author(s):  
W. J. Wang ◽  
R. C. Dalal ◽  
P. W. Moody
Keyword(s):  
Seasonal Variations ◽  
Agricultural Soils ◽  
Cropping System ◽  
Subtropical Climate ◽  
Soil Organic C ◽  
Farming Practices ◽  
Winter Cereal ◽  
Organic C ◽  
Fallow Period

Abstract Agricultural soils play an important role in the global carbon (C) cycling and can act as a significant C sink if managed properly. The long-term (33 years) effects of no till (NT) v. conventional till (CT), stubble retention (SR) v. stubble burning (SB), and N fertiliser application (NF) v. nil N fertilisation (N0) on soil organic C sequestration, and their seasonal variations during the fallow period, were studied in a winter cereal–summer fallow cropping system under semi-arid subtropical climate in Queensland, Australia. The function of different density fractions of soil organic C in determining total organic C (TOC) dynamics and sequestration was investigated. Significant effect of NT, SR, or NF on soil organic C level was observed only in the top 10 cm soil and when they were practiced together, with the TOC contents being 1.1 to 3.4 t/ha higher under NT + NF + SR than under other treatments. There were significant seasonal fluctuations in TOC contents at different stages of the fallow period, and the lowest levels of TOC and treatment effects were observed in the late fallow period. Density fractionation of soil organic C showed that light fraction C (<1.6 g/cm3) declined rapidly during the fallow period and did not accumulate substantially in soil. TOC dynamics, either as a consequence of seasonal variations or as a long-term response to different farming practices, were predominantly controlled by the changes in the heavy fraction C (>1.6 g/cm3).

scholarly journals Cropping system effects on soil quality in the Great Plains: Synthesis from a regional project

2006 ◽  
Vol 21 (1) ◽  
pp. 49-59 ◽  
Author(s):  
B.J. Wienhold ◽  
J.L. Pikul ◽  
M.A. Liebig ◽  
M.M. Mikha ◽  
G.E. Varvel ◽  
...  
Keyword(s):  
Organic Matter ◽  
Soil Properties ◽  
Great Plains ◽  
Management Practices ◽  
Assessment Tool ◽  
Soil Management ◽  
Assessment Tools ◽  
Soil Functions ◽  
Organic C ◽  
Environmental Function

AbstractSoils perform a number of essential functions affecting management goals. Soil functions were assessed by measuring physical, chemical, and biological properties in a regional assessment of conventional (CON) and alternative (ALT) management practices at eight sites within the Great Plains. The results, reported in accompanying papers, provide excellent data for assessing how management practices collectively affect agronomic and environmental soil functions that benefit both farmers and society. Our objective was to use the regional data as an input for two new assessment tools to evaluate their potential and sensitivity for detecting differences (aggradation or degradation) in management systems. The soil management assessment framework (SMAF) and the agro-ecosystem performance assessment tool (AEPAT) were used to score individual soil properties at each location relative to expected conditions based on inherent soil-forming factors and to compute index values that provide an overall assessment of the agronomic and environmental impact of the CON and ALT practices. SMAF index values were positively correlated with grain yield (an agronomic function) and total organic matter (an agronomic and environmental function). They were negatively correlated with soil nitrate concentration at harvest (an indicator of environmental function). There was general agreement between the two assessment tools when used to compare management practices. Users can measure a small number of soil properties and use one of these tools to easily assess the effectiveness of soil management practices. A higher score in either tool identifies more environmentally and agronomically sustainable management. Temporal variability in measured indicators makes dynamic assessments of management practices essential. Water-filled pore space, aggregate stability, particulate organic matter, and microbial biomass were sensitive to management and should be included in studies aimed at improving soil management. Reductions in both tillage and fallow combined with crop rotation has resulted in improved soil function (e.g., nutrient cycling, organic C content, and productivity) throughout the Great Plains.

Wettability of soil aggregates from cultivated and uncultivated Ustolls and Usterts

Soil Research ◽  
2004 ◽  
Vol 42 (2) ◽  
pp. 163 ◽  
Author(s):  
Anna Eynard ◽  
Thomas E. Schumacher ◽  
Michael J. Lindstrom ◽  
Douglas D. Malo ◽  
Robert A. Kohl
Keyword(s):  
Organic Matter ◽  
Great Plains ◽  
Water Intake ◽  
Agricultural Soils ◽  
Water Drop ◽  
Soil Aggregates ◽  
Management Systems ◽  
Northern Great Plains ◽  
Organic C ◽  
Cultivated Soils

Soil organic matter can modify the interaction of clay minerals with water, limiting the rate of water intake of swelling clays and stabilising soil aggregates. Soil structural stability and organic C content usually decrease with cultivation. Faster wetting increases stresses on aggregates and decreases stability. Aggregate wettabilities of prairie soils under 3 different management systems (grassland, no-till, and conventional-till) were compared in the Northern Great Plains of the USA. Six Ustolls and 2 Usterts were selected as replications along the Missouri River. Wettability was measured as water drop penetration time (WDPT) and as rate of water intake under 30 and 300 mm tension. At low tension, aggregates from both cultivated fields and uncultivated grasslands showed similar wettability. Water intake in grass aggregates was attributed to a greater amount of stable pores relative to cultivated aggregates. In cultivated aggregates, slaking created planes of failure that allowed rapid water entry. Differences of wettability between management systems at 300 mm tension (in Ustolls, grasslands had greater wettability than cultivated soils, 0.24 v. 0.17 g water/h.g dry soil) and between soil orders (Usterts had longer WDPT than Ustolls, 2.9 v. 1.7 s) were explained by both clay and organic C contents. Simple measurements of aggregate wettability may be effectively used for soil quality characterisation. Aggregate wettability is a desirable property for agricultural soils when it is related to stable porosity, as may be found in high organic matter soils (e.g. grasslands). Wettability is excessive when fast aggregate wetting results in aggregate destruction as observed in low organic matter cultivated soils.

Soil-Aggregating Bacterial Community as Affected by Irrigation, Tillage, and Cropping System in the Northern Great Plains

Soil Science ◽  
2014 ◽  
Vol 179 (1) ◽  
pp. 11-20 ◽  
Author(s):  
The Can Caesar-TonThat ◽  
William B. Stevens ◽  
Upendra M. Sainju ◽  
Anthony J. Caesar ◽  
Mark West ◽  
...  
Keyword(s):  
Bacterial Community ◽  
Great Plains ◽  
Cropping System ◽  
Northern Great Plains

Impact of tillage on field pea following spring wheat

2009 ◽  
Vol 89 (2) ◽  
pp. 281-288 ◽  
Author(s):  
P. M. Carr ◽  
G. B. Martin ◽  
R. D. Horsley
Keyword(s):  
Great Plains ◽  
Seed Yield ◽  
Spring Wheat ◽  
Water Conservation ◽  
Cropping System ◽  
Field Pea ◽  
Northern Great Plains ◽  
N Fixation ◽  
The Us ◽  
The Impact

Tillage is being reduced in semiarid regions. The impact of changing tillage practices on field pea (Pisum sativum L.) performance has not been considered in a major pea-producing area within the US northern Great Plains. A study was conducted from 2000 through 2005 to determine how field pea performance compared following spring wheat (Triticum aestivum L.) in clean-till (CT), reduced-till (RT), and no-till (NT) systems arranged in a randomized complete block at Dickinson in southwestern North Dakota. Seed yield increased over 1600 kg ha-1 in 2000 and almost 400 kg ha-1 in 2003 under NT compared with CT, and by 960 kg ha-1 in 2000 under NT compared with RT (P < 0.05). Differences in seed yield were not detected between tillage systems in other years. Plant establishment was improved as tillage was reduced, averaging 66 plants m-2 under NT and RT compared with 60 plants m-2 under CT management. The soil water conservation that can occur after adopting NT may explain the increased seed yields that occurred in some years. These results suggest that field pea seed yield can be increased by eliminating tillage in semiarid areas of the US northern Great Plains, particularly when dry conditions develop and persist. Key words: Zero tillage, field pea, cropping system, N-fixation, legume

Cropping system influences on soil chemical properties and soil quality in the Great Plains

2006 ◽  
Vol 21 (1) ◽  
pp. 26-35 ◽  
Author(s):  
M.M. Mikha ◽  
M.F. Vigil ◽  
M.A. Liebig ◽  
R.A. Bowman ◽  
B. McConkey ◽  
...  
Keyword(s):  
Great Plains ◽  
Cropping Systems ◽  
Chemical Properties ◽  
Cropping System ◽  
Soil Chemical Properties ◽  
Total N ◽  
Organic C ◽  
General Chemical ◽  
Study Sites

AbstractSoil management and cropping systems have long-term effects on agronomic and environmental functions. This study examined the influence of contrasting management practices on selected soil chemical properties in eight long-term cropping system studies throughout the Great Plains and the western Corn Belt. For each study, soil organic C (SOC), total N (TN), particulate organic matter (POM), inorganic N, electrical conductivity (EC), and soil pH were evaluated at 0–7.5, 7.5–15, and 15–30 cm within conventional (CON) and alternative (ALT) cropping systems for 4 years (1999–2002). Treatment effects were primarily limited to the surface 7.5 cm of soil. No-tillage (NT) and/or elimination of fallow in ALT cropping systems resulted in significantly (P<0.05) greater SOC and TN at 0–7.5 cm within five of the eight study sites [Akron, Colorado (CO); Bushland, Texas (TX); Fargo, North Dakota (ND); Mandan, ND; and Swift Current, Saskatchewan (SK), Canada]. The same pattern was observed with POM, where POM was significantly (P<0.05) greater at four of the eight study sites [Bushland, TX, Mandan, ND, Sidney, Montana (MT), and Swift Current, SK]. No consistent pattern was observed with soil EC and pH due to management, although soil EC explained almost 60% of the variability in soil NO3-N at 0–7.5 cm across all locations and sampling times. In general, chemical soil properties measured in this study consistently exhibited values more conducive to crop production and environmental quality in ALT cropping systems relative to CON cropping systems.

Effects of 22-year fertilisation on the soil organic C, N, and theirs fractions under a rice-wheat cropping system

2020 ◽  
pp. 1-11
Author(s):  
Yanan Zhao ◽  
Yuting Zhang ◽  
Yueqiang Zhang ◽  
Jun Xie ◽  
Xinping Chen ◽  
...  
Keyword(s):  
Cropping System ◽  
Soil Organic C ◽  
Organic C
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