John Tatarko

Dr. John Tatarko

orcid

Research Focus & Metrics

Academic Career Length

11Years (2016-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 September 2016 in Aeolian Research
Verified
Journal Article
Closed access
NWNicholas Webb
Nicholas Webb
JHJeffrey E. Herrick
Jeffrey E. Herrick
JZJustin W. Van Zee
Justin W. Van Zee
ECEricha M. Courtright
Ericha M. Courtright
CHChristopher H. Hugenholtz
Christopher H. Hugenholtz
LWLarry Wagner
Larry Wagner

11 September 2019 in Earth Surface Processes and Landforms
Verified
Journal Article
Closed access
PDF file
SFStephen E. Fick
Stephen E. Fick
NBNichole Barger
Nichole Barger
JTJohn Tatarko
John Tatarko
MDMichael C. Duniway
Michael C. Duniway

27 October 2017 in GCB Bioenergy
Verified
Journal Article
Open access
YHYuxin He
Yuxin He
DPDeann R Presley
Deann R Presley
JTJohn Tatarko
John Tatarko
HBHumberto Blanco‐Canqui
Humberto Blanco‐Canqui
Crop residue removal can affect the susceptibility to soil wind erosion in climates such as those of the Central Great Plains, United States. Six on‐farm trials were conducted in Kansas from 2011 to 2013 to determine the effects of winter wheat (Triticum aestivumL.), corn (Zea maysL.), and grain sorghum (Sorghum bicolor(L.) Moench), residue removal at 0, 25, 50, 75, and 100% of initial height on soil wind erosion parameters. Those parameters include soil surface random roughness (RR), and wind erodible fraction (EF; aggregates <0.84 mm), geometric mean diameter (GMD) and geometric standard deviation (GSD), stability of dry aggregates (DAS). Complete (100%) residue removal decreased the surfaceRR, increasedEF, and decreasedGMD. OverwinterEFvalues increased for five of six sites from fall 2011 to spring of 2012, particularly for the uppermost removal height (≥75%). MeasuredEF,GMD,GSD,DAS, andRRwere also input into the Single‐event Wind Erosion Evaluation Program (SWEEP) to determine the effect of these parameters on simulated soil loss. TheSWEEPsimulated the wind velocity needed to initiate wind erosion as well as soil loss under each residue removal height at a wind velocity of 13 m s−1for three hours. Threshold wind velocity required to initiate wind erosion generally decreased with increasing crop residue removal height, particularly for >75% removal. Total estimated soil loss over the three‐hour event ranged from ≈2 to 25 Mg ha−1, depending onEF,GMD,GSD,RR, and percent crop residue cover. Removing 75% residue increased simulated wind erosion at three of six sites while removing 50% appears sustainable at all six study sites. Findings reinforce the need for site‐by‐site consideration of the potential amount of crop residue that may be harvested while mitigating wind erosion. Study results indicate the value of maintaining residue at >75% of original height.

15 January 2019
Verified
Book Chapter
Closed access
PDF file
JTJohn Tatarko
John Tatarko
LWLarry Wagner
Larry Wagner
FFFred Fox
Fred Fox

1 December 2016 in Heliyon
Verified
Journal Article
Open access
JTJohn Tatarko
John Tatarko
SDS.J. van Donk
S.J. van Donk
JAJ.C. Ascough
J.C. Ascough
DWD.G. Walker
D.G. Walker
Wind erosion not only affects agricultural productivity but also soil, air, and water quality. Dust and specifically particulate matter ≤10 μm (PM-10) has adverse effects on respiratory health and also reduces visibility along roadways, resulting in auto accidents. The Wind Erosion Prediction System (WEPS) was developed by the USDA-Agricultural Research Service to simulate wind erosion and provide for conservation planning on cultivated agricultural lands. A companion product, known as the Single-Event Wind Erosion Evaluation Program (SWEEP), has also been developed which consists of the stand-alone WEPS erosion submodel combined with a graphical interface to simulate soil loss from single (i.e., daily) wind storm events. In addition to agricultural lands, wind driven dust emissions also occur from other anthropogenic sources such as construction sites, mined and reclaimed areas, landfills, and other disturbed lands. Although developed for agricultural fields, WEPS and SWEEP are useful tools for simulating erosion by wind for non-agricultural lands where typical agricultural practices are not employed. On disturbed lands, WEPS can be applied for simulating long-term (i.e., multi-year) erosion control strategies. SWEEP on the other hand was developed specifically for disturbed lands and can simulate potential soil loss for site- and date-specific planned surface conditions and control practices. This paper presents novel applications of WEPS and SWEEP for developing erosion control strategies on non-agricultural disturbed lands. Erosion control planning with WEPS and SWEEP using water and other dust suppressants, wind barriers, straw mulch, re-vegetation, and other management practices is demonstrated herein through the use of comparative simulation scenarios. The scenarios confirm the efficacy of the WEPS and SWEEP models as valuable tools for supporting the design of erosion control plans for disturbed lands that are not only cost-effective but also incorporate a science-based approach to risk assessment.

1 April 2021 in Soil and Tillage Research
Verified
Journal Article
Closed access
JTJohn Tatarko
John Tatarko
MKMatthew Kucharski
Matthew Kucharski
HLHongli Li
Hongli Li
HLHuiru Li
Huiru Li