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  • 1
    Online Resource
    Online Resource
    American Physical Society (APS) ; 1958
    In:  Physical Review Vol. 110, No. 3 ( 1958-5-1), p. 657-660
    In: Physical Review, American Physical Society (APS), Vol. 110, No. 3 ( 1958-5-1), p. 657-660
    Type of Medium: Online Resource
    ISSN: 0031-899X
    Language: English
    Publisher: American Physical Society (APS)
    Publication Date: 1958
    detail.hit.zdb_id: 2177092-X
    detail.hit.zdb_id: 209766-7
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  • 2
    Online Resource
    Online Resource
    Wiley ; 1990
    In:  Soil Science Society of America Journal Vol. 54, No. 1 ( 1990-01), p. 209-216
    In: Soil Science Society of America Journal, Wiley, Vol. 54, No. 1 ( 1990-01), p. 209-216
    Abstract: A crop model for corn is presented that uses readily available soil, crop, meteorological, and management data as inputs to integrate the effects on grain yield of water stress, plant density, deficit of growing degree days, and planting date. The model can be run on an IBM‐PC, was developed for use in the deep loessial lands of the Upper Mississippi Valley in Major Land Resource Area (MLRA) 105 and associated soil areas, and was calibrated using data for 1972 through 1984 from tillage‐residue management experiments at Lancaster, WI. Estimated water stress, deficit in air‐temperature growing degree days (GDD), and plant density accounted for 77% of the 79% of yield variation explained by the model. The standard error of estimate for predicted yield was 0.67 Mg ha −1 . Presence in the data set of interactions between water stress and GDD, and also water stress with plant density, allowed their incorporation into the model. Tillage and residue management had the principal effects of modifying plant density, soil water storage, and rate of phenologic development to the six‐leaf stage.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1990
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 3
    Online Resource
    Online Resource
    American Physical Society (APS) ; 1966
    In:  Physical Review Vol. 144, No. 1 ( 1966-4-8), p. 295-297
    In: Physical Review, American Physical Society (APS), Vol. 144, No. 1 ( 1966-4-8), p. 295-297
    Type of Medium: Online Resource
    ISSN: 0031-899X
    Language: English
    Publisher: American Physical Society (APS)
    Publication Date: 1966
    detail.hit.zdb_id: 2177092-X
    detail.hit.zdb_id: 209766-7
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  • 4
    Online Resource
    Online Resource
    Wiley ; 1999
    In:  Soil Science Society of America Journal Vol. 63, No. 5 ( 1999-09), p. 1290-1299
    In: Soil Science Society of America Journal, Wiley, Vol. 63, No. 5 ( 1999-09), p. 1290-1299
    Abstract: Nitrate leaching to ground and surface water is an increasing concern in agriculture. Ridge tillage and associated residue management offer potential for modifying the pattern of soil water and solute movement to reduce NO 3 leaching from corn ( Zea mays L.) production. To test this idea we used time domain reflectometry (TDR) measurements of volumetric soil water content (θ) at 0.5‐h intervals following natural rainfall events to determine the pattern of infiltration and soil water recharge for uncropped row and furrow positions in long‐term ridge‐tillage fields. Soil water content was measured under adjacent rows and three adjoining furrows for 103 d in 1992 on a Clarion loam (fine‐loamy, mixed mesic, Typic Hapludoll) near Boone, IA and 96 d on Monona silt loam (fine‐silty, mixed mesic, Typic Hapludoll) near Treynor, IA. During rainfall, infiltration occurred primarily in furrows, as indicated by greater and more rapid initial increases in θ for furrow than for row positions at the same elevation. Following redistribution and evaporation, row and furrow positions at the same elevation had θ values differing by 〈 0.03 m 3 m −3 Changes in profile average θ of rows and furrows between rainfall events were closely correlated ( R 2 〉 0.94). Storage between rainfall events decreased with increasing initial θ and time interval between events ( R 2 〉 0.68), consequently soil water recharge occurred as a series of stepwise increases of θ. These results support the conclusion that water infiltrated in furrows and primarily moved laterally to row positions, minimizing downward water movement under the row. These results explain greater solute movement under furrows than under rows, as found in several short‐term studies.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1999
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 5
    Online Resource
    Online Resource
    New Prairie Press ; 1996
    In:  Conference on Applied Statistics in Agriculture ( 1996-04-28)
    In: Conference on Applied Statistics in Agriculture, New Prairie Press, ( 1996-04-28)
    Type of Medium: Online Resource
    ISSN: 2475-7772
    Language: English
    Publisher: New Prairie Press
    Publication Date: 1996
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  • 6
    Online Resource
    Online Resource
    Wiley ; 1963
    In:  Soil Science Society of America Journal Vol. 27, No. 4 ( 1963-07), p. 478-481
    In: Soil Science Society of America Journal, Wiley, Vol. 27, No. 4 ( 1963-07), p. 478-481
    Type of Medium: Online Resource
    ISSN: 0361-5995
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1963
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
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  • 7
    Online Resource
    Online Resource
    Wiley ; 1999
    In:  Soil Science Society of America Journal Vol. 63, No. 2 ( 1999-03), p. 264-269
    In: Soil Science Society of America Journal, Wiley, Vol. 63, No. 2 ( 1999-03), p. 264-269
    Abstract: Point injection of N fertilizers within the ridge of ridge‐tilled soils has shown promise in reducing nitrate leaching in short‐term rainfall simulation studies, but it has not been studied under natural rainfall throughout the growing season. At two uncropped locations, we measured the leaching of tracers injected into different ridge positions in established ridge‐tilled plots that were leached by natural rainfall. A point injector was used to inject conservative anionic tracers 100 mm below the soil surface every 38.1 mm along ridge‐top, ridge‐shoulder, and furrow positions. Movement of tracers was measured four times after tracer application by triplicate soil sampling with a 38.1‐mm‐diam. soil probe to a maximum depth of 1.22 m. Sample collection spanned a period of 102 d with 282 mm of cumulative precipitation after tracer application at the Boone site and 97 d with 314 mm of precipitation at the Treynor site. Mass recoveries of furrow‐applied tracer was significantly lower ( P = 0.05) than ridge‐applied tracer on the last two sampling dates at both sites. There was no consistent difference in mass recoveries between tracers applied at ridge top compared with shoulder positions. Furrow‐applied tracer had lower concentrations in the soil profile than tracers applied to ridge‐top and shoulder positions after 40 d and 76 to 129 mm of precipitation. Tracer movement was essentially vertical below the ridges, with ≥96% of the recovered ridge‐applied tracer found below the ridges. Lateral spreading was more pronounced under the furrows, with ≥49% of the recovered furrow‐placed tracer found below the furrows. Fertilizer injection within the ridge shows promise for reducing leaching and potentially increasing nutrient availability to plants.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1999
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
    Location Call Number Limitation Availability
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  • 8
    In: Physical Review A, American Physical Society (APS), Vol. 40, No. 11 ( 1989-12-1), p. 6169-6184
    Type of Medium: Online Resource
    ISSN: 0556-2791
    RVK:
    Language: English
    Publisher: American Physical Society (APS)
    Publication Date: 1989
    detail.hit.zdb_id: 2844156-4
    detail.hit.zdb_id: 209769-2
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  • 9
    Online Resource
    Online Resource
    Wiley ; 1993
    In:  Soil Science Society of America Journal Vol. 57, No. 4 ( 1993-07), p. 917-923
    In: Soil Science Society of America Journal, Wiley, Vol. 57, No. 4 ( 1993-07), p. 917-923
    Abstract: The borehole permeameter technique can produce erratic saturated hydraulic conductivity ( K sat ) in soils with macropores and abrupt layers because operating theory assumes homogeneous and isotropic conditions. Dye application during an infiltration test demonstrated water movement in macropores and erratic K sat or matric flux potential (ϕ m ). To evaluate the effects of macropores, cracks, and layered soil on K sat and ϕ m , a finite element solution of the Richards equation was used to simulate infiltration from a borehole (0.03‐m radius and 0.50 m deep) with a constant head ( H ) of 0.05 or 0.10 m. Borehole infiltration (for 2 h) was simulated for a Rozetta silt loam (fine‐silty, mixed, mesic Typic Hapludalf) with four configurations: homogeneous, layered, a cylindrical macropore centered at the borehole base, and a crack intersecting the borehole wall. Simulated flow rates were increased by 29% (with H = 0.05 m) and 21% (with H = 0.10 m) when a cylindrical macropore (4 mm by 0.10 m) was located at the borehole base. Respective increases were 25% ( H = 0.05 m) and 20% ( H = 0.10 m) when a crack extending 0.1 m laterally intersected the borehole wall. Three methods were tested for calculating K sat . The simultaneous‐equations approach (SEA) using either the Guelph or the Philip model for a homogeneously configured borehole estimated K sat within a factor of 2 from input K sat , but the Laplace analysis method overestimated input K sat by a factor of 5 to 12. The fixed α value (α = K sat /ϕ m ) method with either the Guelph or Philip model estimated K sat close to input K sat when a proper α value was chosen, but the proper α value differed by soil and model. A negative K sat was computed using the SEA with the Guelph model when macropores intersected the base of a borehole; negative K sat or ϕ m were produced when cylindrical macropores laterally intersected the borehole wall, depending on the vertical locations of the macropores. Soil with layered hydraulic properties also produced unrealistic K sat .
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1993
    detail.hit.zdb_id: 241415-6
    detail.hit.zdb_id: 2239747-4
    detail.hit.zdb_id: 196788-5
    detail.hit.zdb_id: 1481691-X
    SSG: 13
    SSG: 21
    Location Call Number Limitation Availability
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  • 10
    Online Resource
    Online Resource
    American Physical Society (APS) ; 1959
    In:  Physical Review Vol. 116, No. 1 ( 1959-10-1), p. 81-83
    In: Physical Review, American Physical Society (APS), Vol. 116, No. 1 ( 1959-10-1), p. 81-83
    Type of Medium: Online Resource
    ISSN: 0031-899X
    Language: English
    Publisher: American Physical Society (APS)
    Publication Date: 1959
    detail.hit.zdb_id: 2177092-X
    detail.hit.zdb_id: 209766-7
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