Soil Dissipation and Runoff Losses of the Herbicide Pendimethalin in Tobacco Field

2009 ◽  
Vol 201 (1-4) ◽  
pp. 253-264 ◽  
Author(s):  
Vasilios Triantafyllidis ◽  
Dimitra Hela ◽  
George Salachas ◽  
Panayiotis Dimopoulos ◽  
Triantafyllos Albanis
Weed Science ◽  
2006 ◽  
Vol 54 (4) ◽  
pp. 800-806 ◽  
Author(s):  
David R. Shaw ◽  
Stephen M. Schraer ◽  
Joby M. Prince ◽  
Michele Boyette ◽  
William L. Kingery

The effects of time of precipitation and soil type on runoff losses of cyanazine and metolachlor were studied using a tilted-bed, microplot system. Two silt loam soils, Bosket and Dubbs, and a Sharkey silty clay were evaluated. Rainfall (22 mm h−1) was simulated at 0, 2, and 14 days after treatment (DAT). Time of precipitation did not impact herbicide losses or any of the runoff parameters evaluated in this study. Water runoff occurred sooner and in greater quantities from the surfaces of Bosket and Dubbs silt loam soils than from the surface of Sharkey silty clay. Runoff losses of cyanazine did not vary by soil type. Soil drying produced large cracks in Sharkey silty clay, which greatly reduced runoff in this soil. Combined runoff and leachate losses were highest from Dubbs silt loam. Runoff losses of metolachlor were not affected by soil type. However, regression analyses indicated that time of precipitation and soil type interacted to affect initial metolachlor concentration. At 14 DAT, initial metolachlor concentration was highest in runoff from Sharkey soil. Time of precipitation ranked with respect to initial metolachlor concentration in runoff from Bosket and Dubbs silt loam soils were 0 > 2 > 14 DAT and 0 = 2 > 14 DAT, respectively.


1991 ◽  
Vol 37 (4) ◽  
pp. 303-314 ◽  
Author(s):  
J.K. Hall ◽  
R.O. Mumma ◽  
D.W. Watts
Keyword(s):  

1994 ◽  
Vol 74 (1) ◽  
pp. 59-66 ◽  
Author(s):  
B. T. Bowman ◽  
G. J. Wall ◽  
D. J. King

The risk of surface-water contamination by herbicides is greatest following application to cropland when the active ingredients are at the maximum concentration and the soil is the most vulnerable to erosion following cultivation. This study determined the magnitude of surface runoff losses of herbicide and nutrients at, and subsequent to, application. The first of three weekly 10-min, 2.6-cm rainfalls were simulated on triplicated 1-m plots (a set) on which corn had been planted and the herbicide (metolachlor/atrazine, 1.5:1.0) and fertilizer (28% N at 123 kg ha−1) had just been applied. Identical simulations were applied to two other adjacent plot sets (protected from rainfall) 1 and 2 wk following herbicide application. Runoff (natural, simulated) was monitored for soil, nutrient and herbicide losses. Concentrations of total phosphorus in surface runoff water and nitrate N in field-filtered samples were not significantly influenced by the time of the rainfall simulation but exceeded provincial water-quality objectives. Atrazine and metolachlor runoff losses were greatest from simulated rainfall (about 5% loss) immediately following application. Subsequent simulated rainfall usually resulted in < 1% herbicide runoff losses. Herbicide concentrations in all plot runoff samples exceeded provincial drinking-water quality objectives. Since herbicide surface transport is primarily in the solution phase (not via association with soil particles), water-management conservation technologies are the key to retaining these chemicals on cropland. Key words: Herbicide, runoff, rainfall simulation, partitioning, water quality


2014 ◽  
Vol 43 (2) ◽  
pp. 549-557 ◽  
Author(s):  
Inoka D. Amarakoon ◽  
Francis Zvomuya ◽  
Allan J. Cessna ◽  
Dani Degenhardt ◽  
Francis J. Larney ◽  
...  

2011 ◽  
Vol 40 (2) ◽  
pp. 412-420 ◽  
Author(s):  
Leonard C. Kibet ◽  
Arthur L. Allen ◽  
Peter J. A. Kleinman ◽  
Gary W. Feyereisen ◽  
Clinton Church ◽  
...  

2008 ◽  
Vol 171 (2) ◽  
pp. 187-192 ◽  
Author(s):  
Surjit Kaur Dhillon ◽  
Karaj Singh Dhillon ◽  
Anshuman Kohli ◽  
Kishan Lal Khera

1982 ◽  
Vol 74 (6) ◽  
pp. 947-950 ◽  
Author(s):  
K. W. Brown ◽  
J. C. Thomas ◽  
R. L. Duble

2019 ◽  
Author(s):  
Shuang He ◽  
Fayong Li ◽  
Xinqiang Liang ◽  
Hua Li ◽  
Sheng Wang ◽  
...  

Abstract Background Rice paddy wetlands may serve as a nutrient source or sink in agricultural ecosystems. However, the pattern of nutrient loss on a large scale is not clear. A year-round on-site observation study based on 6 h intervals was conducted. Rainfall, temperature, runoff nutrient concentrations, and adjacent stream water samples were automatically monitored to uncover the temporal changes in the runoff losses of the main nutrient proxies (total N and total P) from a typical rice-planting area (120 ha) in the Yangtze river delta region of China.Results A high total N concentration in the rice-planting area was observed during the rice-planting season; however, a larger fluctuation in the total P was evident throughout the year. The Δtotal N (drainage minus stream) parameter showed negative values with a mean of −0.25 mg L −1 , while Δtotal P showed positive values with a mean of 0.06 mg L −1 . The window phases for the total N loss are mainly concentrated in the rice-growing season. However, the window phase for the total P loss was more dispersive throughout the year. No clear relationships were found between rainfall and N and P concentrations by self-organizing map analysis.Conclusions This high-resolution monitoring suggested that nutrient loss loading, rather than nutrient concentration, was strongly related to runoff depth, and the avoidance of fertilization before high-intensity rainfall could mitigate the nutrient runoff losses and maintain the rice wetland eco-function.


2021 ◽  
Author(s):  
Jose Alfonso Gomez ◽  
Gema Guzman

&lt;p&gt;Maintenance of ground cover vegetation in olive orchards has been shown to reduce soil and runoff losses as compared to bare soil. However, extrapolation of its impact at hillslope scale under different conditions still challenging for several reasons. One is the limited duration of available experiments, usually shorter than 3 years, which can&amp;#180;t capture the annual variability in precipitation typical of Mediterranean type of climate. A second reason is the small scale in which many experiments are carried out, which do not capture all the relevant erosion processes at hillslope scale. A third reason, hardly discussed, is the use of the runoff plots that limits traffic resulting in conditions that might not be fully representative of actual orchards.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;&lt;p&gt;For evaluating the effect of temporary cover crops on water erosion processes in olives at hillslope scale, runoff and soil losses have been monitored from 2008 to 2019 in La Conchuela. This is an olive farm located in Southern Spain, where average annual precipitation is 655 mm, on Typic Haploxerert (clay content &gt; 50%). Six runoff plots (14x24 m) delimited by steel beams on concrete foundation were established in a 13.4 % slope, containing 3 rows of 4 trees. This allows normal farm operations. Since 2008-2009, two soil management systems, conventional tillage (CT) and temporary cover crops (CC), were tested. In the two CT plots ground vegetation was controlled by 2-3chisel ploughing passes during the year. CC in the other four plots consisted of sowing manually in mid Fall a grass or a mix with grasses every 1 to 3 years without disturbing the soil surface, been mowed in early Spring. The aim of this cover crop was to be grown up spontaneously from seed produced the previous year. Weeds along the tree rows are controlled by herbicides in both cases.&lt;/p&gt;&lt;p&gt;No significant differences were detected (p &lt; 0.05) for the whole period, although CC showed lower runoff and soil losses values. Runoff data ranged from 157.7 &amp;#177; 61.2 to 144.5 &amp;#177; 46.4 mm, and soil losses varied from 24.3 &amp;#177; 9.1 to 16.4 &amp;#177; 7.0 t&amp;#183;ha&lt;sup&gt;-1&lt;/sup&gt; at the CT and CC treatments respectively. The lack of statistical differences can be explained by the large variability recorded in the measurements at the six plots, especially at the CC due to the specific weather and traffic conditions. Our experiment shows how in a crop, olives, subject to intense traffic during the harvesting season (happening in late fall or early winter, rainy season) and in an orchard on heavy soils, maintenance of a good cover crop is challenging in many years. Our results call for caution when extrapolating the benefits of cover crops in olives from the experimental plots to real world conditions. It also highlights the need for improved soil management under these conditions (e.g. controlled traffic, combination with inert mulch, &amp;#8230;) to improve soil and water conservation in intensively cultivated olive orchards in heavy soils.&lt;/p&gt;&lt;p&gt;&amp;#160;&lt;/p&gt;


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