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  • 1
    Online Resource
    Online Resource
    Wiley ; 1983
    In:  Soil Science Society of America Journal Vol. 47, No. 4 ( 1983-07), p. 810-817
    In: Soil Science Society of America Journal, Wiley, Vol. 47, No. 4 ( 1983-07), p. 810-817
    Abstract: Efficient N applications are necessary to maximize bermudagrass ( Cynodon dactylon L.) dry matter yield and N uptake in forage. Significant losses of NH 3 from surface applications of urea and NH 4 ‐N fertilizers by volatilization have been reported. Field experiments were conducted over a three‐year period under a wide range of climatic and soil conditions in Oklahoma to determine the efficiency of N applications for dry matter production and N uptake in bermudagrass forage. Four locations were selected in 1978 and one each in 1979 and 1980, representing four typical soil types for bermudagrass production with a pH range of 4.7 to 6.9. Anhydrous ammonia (AA) and ammonia passed through a Cold‐Flo adapter (ACF) were injected into bermudagrass sod and urea‐ammonium‐nitrate (UAN), urea, and (NH 4 ) 2 SO 4 (AS) were broadcast. Rates of N were 0, 112, 224, and 448 kg·ha −1 initially as well as 224, 336, and 448 kg·ha −1 in split applications. An additional experiment was established in 1980 to evaluate the effect of S on yield and N uptake. Rates of S were 0 and 64 kg · ha −1 and sources were elemental S, CaSO 4 · 2H 2 0, MgSO 4 , and AS. There were two harvests at each location in 1978, three in 1979, and two in 1980. Yield and N uptake from AA and ACF applications were not significantly different, but generally were lower than with broadcast UAN, urea, and AS. Yield and N uptake generally were lower from urea than UAN and AS. Relative efficiency of N sources obtained from averaging across N response experiments were in the order of AS 〉 UAN 〉 urea 〉 AA 〉 ACF. Split application of N in 1978 and 1980 did not increase yield, but in 1979 an increase in yield was obtained with more even rainfall distribution during the growing season. Sulfur fertilization decreased N:S ratios in forage, but did not increase yield or N uptake or improve N efficiency. Potential losses of NH 3 by volatilization from broadcast urea, UAN, and AS in these experiments were considered minimal.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1983
    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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  • 2
    Online Resource
    Online Resource
    Wiley ; 1972
    In:  Soil Science Society of America Journal Vol. 36, No. 1 ( 1972-01), p. 82-86
    In: Soil Science Society of America Journal, Wiley, Vol. 36, No. 1 ( 1972-01), p. 82-86
    Abstract: Urea and oxamide, each labeled with 15 N, were compared as fertilizers in two field experiments in adjacent locations in successive years with ‘Sudax SX11’ Sorghum‐sudan hybrid ( Sorghum sudanense ) as the test crop. Four cuttings were harvested during the first experiment and three during the second. Patterns of uptake of fertilizer N were in accord with the characteristics of the two carriers. In the first harvests in both experiments the amounts of N taken up from urea were markedly greater than from oxamide; but by the third harvests, yield responses and N uptake from oxamide were greater than from urea. Total recoveries of fertilizer N from the two carriers during the entire growing season were similar as greater recoveries of urea‐N in the early summer were compensated for by greater recoveries of oxamide‐N in the late summer. Of the N added in urea in the first experiment, 51% was recovered in the crops and 28% was still in the soil (0–25cm) at the end of the growing season. Corresponding figures for oxamide were 52% in the crops and 31% in the soil. In the second experiment, when fertilizer applications and planting operations were delayed until more favorable growing weather, 93% and 99% of the urea‐ and oxamide‐N, respectively, were estimated as recovered in the crops, and measurements of the amounts of fertilizer remaining in the soil were not attempted.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1972
    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
    Wiley ; 1994
    In:  Agronomy Journal Vol. 86, No. 6 ( 1994-11), p. 1016-1019
    In: Agronomy Journal, Wiley, Vol. 86, No. 6 ( 1994-11), p. 1016-1019
    Abstract: Stability analysis, which is the linear regression of treatment yield on the environmental mean yield, has been proposed for use in singlesite, long‐term experiments (treatments applied to the same plots year after year), without first determining if treatment yield reveals a significant relationship with year (experiment years plotted sequentially in time). This research was initiated to demonstrate potential problems associated with stability analysis on long‐term, wheat fertility experiments where treatment yield may be correlated with year. Three single‐site, long‐term experiments were evaluated using stability analysis and linear regression of treatment yield on year. Each study was a replicated, longterm, continuous winter wheat ( Triticum aestivum L.) fertility experiment, receiving annual rates of N, P, and K fertilizer. Of the single‐site, long‐term trials evaluated, one was not suitable for stability analysis, as grain yield decreased significantly with each ensuing year that the experiment was conducted. In this case, a negative residual yield response was noted with time (year) in plots receiving N and no P. Therefore, the environmental mean in stability analysis no longer reflected the random influence of climate (e.g., low and high rainfall or temperature) which could be used to decipher variable treatment response in seasonably wet or dry years. Without prior evaluation of the relationship between treatment yield and year in single‐site, long‐term experiments, stability analysis can be inappropriate.
    Type of Medium: Online Resource
    ISSN: 0002-1962 , 1435-0645
    Language: English
    Publisher: Wiley
    Publication Date: 1994
    detail.hit.zdb_id: 1471598-3
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  • 4
    Online Resource
    Online Resource
    Wiley ; 1997
    In:  Journal of Production Agriculture Vol. 10, No. 4 ( 1997-10), p. 580-585
    In: Journal of Production Agriculture, Wiley, Vol. 10, No. 4 ( 1997-10), p. 580-585
    Type of Medium: Online Resource
    ISSN: 0890-8524 , 2689-4114
    Language: English
    Publisher: Wiley
    Publication Date: 1997
    detail.hit.zdb_id: 2806272-3
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  • 5
    Online Resource
    Online Resource
    Wiley ; 1995
    In:  Journal of Production Agriculture Vol. 8, No. 4 ( 1995-10), p. 584-589
    In: Journal of Production Agriculture, Wiley, Vol. 8, No. 4 ( 1995-10), p. 584-589
    Type of Medium: Online Resource
    ISSN: 0890-8524
    Language: English
    Publisher: Wiley
    Publication Date: 1995
    detail.hit.zdb_id: 2806272-3
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  • 6
    Online Resource
    Online Resource
    Wiley ; 1991
    In:  Agronomy Journal Vol. 83, No. 1 ( 1991-01), p. 24-29
    In: Agronomy Journal, Wiley, Vol. 83, No. 1 ( 1991-01), p. 24-29
    Abstract: Renewed interest in low‐input and sustainable crop production has rekindled interest in long‐term agronomic research. Research plots that have been monitored continuously since the late 19th Century exist in several states. Twenty‐five experiments have been identified that have been monitored for over 25 yr; 12 of these are more than 50 yr old. Yield and treatment records provide valuable information on the effects of cropping systems, tillage, manuring, and fertilization practices on yields and on soil physical and chemical properties, Most of these very early tests were non‐replicated studies using large plots and crop rotation systems. Four of America's oldest, continuous agronomic research tests were reviewed in more detail: (i) Illinois' “Morrow Plots” (c. 1876), (ii) Missouri's “Sanborn Field” (c. 1888), (iii) Oklahoma's “Magruder Plots” (c. 1892) and (iv) Alabama's “Old Rotation” (c. 1896). All of these are listed on the National Register of Historical Places. These studies document that long‐term crop production can be sustained and improved in different regions and on different soils of the USA. Long‐term studies have shown that crop rotations and attention to recognized and established soil fertility practices, which may or may not include legumes and manuring, are essential to maintaining high, sustained production.
    Type of Medium: Online Resource
    ISSN: 0002-1962 , 1435-0645
    Language: English
    Publisher: Wiley
    Publication Date: 1991
    detail.hit.zdb_id: 1471598-3
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  • 7
    Online Resource
    Online Resource
    Wiley ; 1986
    In:  Soil Science Society of America Journal Vol. 50, No. 6 ( 1986-11), p. 1606-1613
    In: Soil Science Society of America Journal, Wiley, Vol. 50, No. 6 ( 1986-11), p. 1606-1613
    Abstract: Current changes in residue management systems for winter wheat ( Triticum aestivum L.) include anhydrous NH 3 injection combined with herbicide application, planting, and other field operations. The feasibility of NH 3 application during planting is dependent upon potential NH 3 toxicity to germinating seeds. A laboratory experiment was conducted to study anhydrous NH 3 movement in soils by injecting 124 and 180 mg N as NH 3 into a Hollister clay (fine, mixed, thermic Pachic Paleustolls), Grant silt loam (fine‐silty, mixed, thermic Udic Argiustolls), and Norge clay loam (fine‐silty, mixed, thermic Udic Paleustolls) at 0.124 and 0.181 water (kg kg −1 ) contents. Soil samples were taken 1, 7, and 14 d after N application. Soil NH + 4 ‐N and calculated NH 3 (aq) concentrations following NH 3 injection generated a normal distribution curve with N concentrations highest near the injection point and decreasing with increasing distance. Calculated NH + 4 diffusion coefficients decreased with time and water content and were soil dependent. Field studies were conducted in 1983 to determine the potential germination hazard from NH 3 applied at 0, 56, 112, 168, 224, and 280 kg N ha −1 while planting, and in 1984 to winter wheat planted 0, 1, 3, 5, 6, and 7 d after applications of 0, 100, and 200 kg N ha −1 . Stand counts, forage NO ‐ 3 ‐N concentration, and yield were not influenced by NH 3 applications during planting in 1983, but grain N concentration increased linearly up to 24.1 mg g −1 with 280 kg N ha −1 . In the 1984 experiment, increasing NH 3 rates did not decrease seedling stand, even though analysis of soil samples reflected increased soil pH and soil NH + 4 ‐N concentration. Anhydrous NH 3 placement at a sufficient distance from newly seeded rows will ensure the success of systems which include NH 3 injection in conjunction with other field operations in residue management systems.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1986
    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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  • 8
    Online Resource
    Online Resource
    Wiley ; 1973
    In:  Soil Science Society of America Journal Vol. 37, No. 5 ( 1973-09), p. 725-727
    In: Soil Science Society of America Journal, Wiley, Vol. 37, No. 5 ( 1973-09), p. 725-727
    Abstract: Evidence of the “priming effect” on the uptake of soil N by additions of rather conservative amounts of fertilizer N was examined in data from two recently reported field experiments. In these experiments, urea and oxamide each labeled with 15 N were compared on adjacent locations in successive years with ‘Sudax SX11’ Sorghum‐sudan hybrid ( Sorghum sudanense ) as the test crop. The priming effect in the first experiment was calculated from data from four cuttings during the first year and from a residual cutting during the second year. For the second experiment, data were used from the three cuttings harvested during the year the fertilizers were applied. Additions of N fertilizer increased the uptake of soil N by 17 to 45% in the first experiment in 1966 and by 8 to 27% in the second experiment in 1967. In the residual cutting of the first experiment, increases in uptake of soil N ranged from less than 0 to 29%. The increase in uptake of soil N by the crops was speculated to be due to stimulation of microbial activity by N fertilizers which increased mineralization of soil N, thus making more soil N available for use by plants.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1973
    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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  • 9
    Online Resource
    Online Resource
    Wiley ; 1972
    In:  Soil Science Society of America Journal Vol. 36, No. 1 ( 1972-01), p. 91-94
    In: Soil Science Society of America Journal, Wiley, Vol. 36, No. 1 ( 1972-01), p. 91-94
    Abstract: Residual effects of two 15 N‐labeled N fertilizers, urea and oxamide, were compared during the second cropping season after they had been applied at rates of 0, 56, 112, and 168 kg N/ha. ‘Sudax SX11’ sorghum‐sudan grass hybrid ( Sorghum sudanense ) was grown and harvested three times during this second cropping season while the residual effects were being measured. Fertilizer N removed in plant tops during this second year of cropping contained 13–18% of the residual fertilizer N in the soil at the end of the first season and was equal to 4–6% of that applied originally in the fertilizers. At the end of the second cropping season, 22 and 26% of the initial applications of N in urea and oxamide, respectively, remained in the soil. The effect of carriers on these amounts of residual fertilizer N was not significant. The removals in crops during the second season plus those amounts remaining in the soil at the end of the second season were essentially equal to the residual fertilizer N which had been in the soil at the end of the first season. Thus, no evidence was found for loss of residual N by leaching, denitrification, or other processes during the second cropping season. Since removals of N in crops were considerably greater than the additions in fertilizers, it is hypothesized that nearly all inorganic fertilizer N was taken out of the soil and most of the residual fertilizer N was in relatively stable organic forms. Conditions for these experiments had been selected to conserve N, and as a consequence the deficits of fertilizer N reported here may be expected to be smaller than might occur under other practices.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1972
    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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  • 10
    Online Resource
    Online Resource
    Wiley ; 1984
    In:  Soil Science Society of America Journal Vol. 48, No. 6 ( 1984-11), p. 1292-1296
    In: Soil Science Society of America Journal, Wiley, Vol. 48, No. 6 ( 1984-11), p. 1292-1296
    Abstract: Arrowleaf clover ( Trifolium vesiculosum Savi ‘Yuchi’) is a winter annual legume that can be used to extend the grazing of warm‐season perennial grasses in forage production systems. Stand establishment from overseeding often fails because of unfavorable climatic conditions and nutrient deficiencies in soils. The objectives of this research were to determine the effects of P and K fertilization on yield and nutrient uptake of arrowleaf clover and accumulation of soil P and K. Arrowleaf clover was seeded in field plots in the fall of 1978. Fertilizer treatments consisted of an incomplete factorial arrangement of multiple rates of P, K, and P plus K. Rates of P and K included a control that did not receive fertilizer; 20, 40, and 80 kg P ha −1 ; 37, 74, and 148 kg K ha −1 ; and P‐K combinations of 20:37, 40:74, and 80:148 kg ha −1 . The soil type was a Taloka silt loam (Mollic Albaqualfs). Yield and N, P, and K uptake in forage were determined in four consecutive years starting in 1979. Soil test indices were measured prior to seeding in 1977, in the fall of 1978, and after four annual fertilizations in 1982. Regression equations with linear, quadratic, and interaction terms were calculated to describe dependent variable response surfaces for each year and the average over years. Phosphorus fertilization increased yield each year. Yield was not increased with K fertilization alone, but there was a positive P × K interaction in the 1982 season indicating soil K levels were decreasing. Predicted maximum yields were 6561, 6490, 6516, and 6860 kg ha −1 due to applications of 50.8, 52.4, 54.0 and 57.2 kg P ha −1 , respectively, at fixed rates of 0, 37, 74, and 148 kg K ha −1 . Phosphorus increased N, P, and K uptake and when applied in combinations with K, some interactions occurred. The soil test index for P increased slowly (0.5 kg ha −1 yr −1 ) with P rates of 20 kg ha −1 annually; however, a rapid accumulation of soil P occurred with four annual applications of 80 kg P ha −1 (16.5 kg ha −1 yr −1 ). Approximately 107, 16, 6, and 3 annual applications of 20, 40, 60, and 80 kg P ha −1 , respectively, would be required to increase soil test values for P to a sufficient level. Soil test values for K were increased from 133 to 308 kg ha −1 with four annual applications of 148 kg K ha −1 . However, after four annual applications of 80 kg P ha −1 in combination with 148 kg K ha −1 , the soil test value for K was only increased to 192 kg ha −1 due to the marked response from P fertilization and subsequent increase of K removal in forage.
    Type of Medium: Online Resource
    ISSN: 0361-5995 , 1435-0661
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1984
    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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