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GIS Approach to Estimate Windbreak Crop Yield Effects in Kansas–Nebraska

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GIS Approach to Estimate Windbreak Crop Yield Effects in Kansas–Nebraska Agroforest Syst https://doi.org/10.1007/s10457-018-0270-2 (0123456789().,-volV)(0123456789().,-volV) GIS approach to estimate windbreak crop yield effects in Kansas–Nebraska Rau´l J. Osorio . Charles J. Barden . Ignacio A. Ciampitti Received: 10 February 2018 / Accepted: 27 June 2018 Ó The Author(s) 2018 Abstract Windbreaks were originally promoted area taken out of crop production. Results showed: across the U.S. Great Plains to reduce wind erosion. soybeans (57 crop/years) presented the most positive A review paper published nearly 30 years ago showed response to windbreak effect with significant yield yield increases for a variety of crops associated with increases 46% of the time, with a 16% (283 kg ha-1) windbreaks. However, with the widespread use of no- average yield increase. Wheat (44 crop/years) yield till cropping systems and advanced crop genetics, the increases were significant 30% of the time, with a 10% question is ‘‘Do windbreaks still provide a yield (319 kg ha-1) average yield increase. Narrow wind- benefit?’’ This study compared data from protected breaks (1–2 tree rows, average width of 13 m) and and unprotected fields over multiple years across those on the north edge of fields resulted in yield Kansas and Nebraska looking at relative soybean increases that compensated for the footprint of the (Glycine max L.) and winter wheat (Triticum aestivum windbreak more often (71%) than wider windbreaks L.) yield differences. Farmer’s pre-existing georefer- on the south edges of fields (38%). enced data, generated by automated combine yield monitors, were analyzed with ArcGIS 10.3.1 to Keywords Windbreak effects Á Soybeans Á Wheat Á visualize windbreak interaction with crop yield. Shelterbelts Á Agroforestry Statistics were conducted to determine if the yield in protected areas of the field was significantly different from the yield in unprotected areas. Also, yield loss was estimated from the windbreak footprint to assess Introduction if yield increases were enough to compensate for the Windbreaks were widely promoted and established across the Great Plains region of the U.S. to reduce R. J. Osorio (&) Á C. J. Barden wind erosion, following the 1930s Dust Bowl that Department of Horticulture and Natural Resources, damaged the U.S. and Canadian agricultural prairies College of Agriculture, Kansas State University, 2021 (Hansen and Libecap 2004). The U.S. Congress Throckmorton Hall, 1712 Claflin Rd, Manhattan, KS 66506, USA financed the Prairie States Forestry Project, through e-mail: [email protected] the U.S. Forest Service (Droze 1977). A total of 250 million trees were planted in 30,000 windbreaks with a I. A. Ciampitti total length of 29,900 km from Texas to Canada, by Department of Agronomy, College of Agriculture, Kansas State University, 2021 Throckmorton Hall, 1712 Claflin 1942, in a 160-km wide zone (Droze 1977; Croker Rd, Manhattan, KS 66506, USA 123 Agroforest Syst 1991). Field windbreaks are considered to be part of a field windbreak, which subtracts yield loss due to sustainable agricultural system consisting of single or windbreak competition from the yield gain due to multiple lines of trees and shrubs planted along the windbreak protection to estimate the net windbreak edge of agriculture lands mainly to reduce the wind effect. In this study, we also consider that the potential erosion and provide protection to field crops (Brandle yield of the windbreak footprint also needs to be et al. 2004). subtracted, to estimate the total impact on yield from In Kansas, the most recent windbreak assessment the windbreak (Fig. 1). was conducted by the Great Plains Initiative in 2008 Previous research demonstrated that most yield and 2009. Moser et al. (2008) using GIS across multi- increase due to windbreaks occur within 10 H in the county regions, reported an estimate of 289,577 downwind zone, or within 0–3 H in the windward side windbreaks with a length of 69,900 km protecting (Grace 1977; Kort 1988; Baldwin 1988) The world 0.49 million hectares of land. Ghimire et al. (2014) data compilation done by Kort (1988) showed yield estimated that 44% of Kansas windbreaks were in fair increases from 0.5–13 H on the leeward side of the to poor condition. In this research, only windbreaks in field. Sudmeyer and Scott (2002) reported that good conditions were considered, with most of the regardless of the season, crops in the downwind windbreaks (87%) being located in Kansas. protected zone from 3 to 20 times the windbreak H The first and main parameter to consider before presented an increase in yield of 16–30% relative to planting a windbreak is orientation. Windbreaks are the unprotected area beyond 30 times the H of the effective when they are located perpendicular to the windbreak. It has generally been confirmed that prevailing wind direction (Tamang et al. 2015). maximum yield gains are usually found between 3 Careful species selection depending on the soil-site and 10 H in the quiet zone, which is the zone conditions and designing the windbreak to reduce its immediately behind the windbreak (Cleugh 1998). width, maximizes crop yield benefits (Kort 1988). Yield reductions can also occur, according to Stoeck- Also, optimal crop yield increases are achieved when eler (1962), with a potential negative impact for crops narrow windbreaks have dense to medium porosity, closer than 1.5 H from the windbreak. consisting of fast-growing and non-competitive trees Crop yield reductions close to the vegetative species (Kort 1988). Several tall, long-lived species barriers result from a combination of above-and with deep root systems and similar growth should be below-ground competition between shelterbelts and planted. crops (Brenner et al. 1993). According to Stoeckeler Two primary factors that determine windbreak (1962) competition between tree and crop roots for effectiveness in reduction of wind speed are the soil moisture and shading is likely the primary cause windbreak height and porosity. Windbreak height for yield reductions adjacent to windbreaks. Other determines the horizontal extent of the sheltered area reasons for crop yield reductions include allelopathy, (Koh et al. 2014). According to Heisler and Dewalle increased temperatures, and nutrient leaching after (1988) upwind and downwind effects are usually heavy snow accumulation (Kort 1988; Andrue et al. assumed to be proportional to windbreak height, noted 2009). Greb and Black (1961) reported that moisture as H in formulas and models. Reductions of wind content of the area is a key factor that affects the speed have been recorded as far as 50 H to the leeward competition between crops and windbreaks. Crop type zone (Naegeli 1964; Monteith 1973) and reductions of is another factor to consider in the effect of a about 20% may extend to about 25 H from the windbreak. In one study wheat (Triticum) and oats windbreak (Naegeli 1946). The protected zone on the (Avena sativa) showed larger losses in the zone close windward side is in the range of 2–5 H. On the leeward to the barrier (Bates 1944). Other important reasons side the peak protected zone is usually between 6 and that explain crop yield increases in the protected zone 10 H and extends to about 15 H downwind (Brandle are reduction in leaf abrasion, stripping and tearing of et al. 2009). Most benefits occur within 10 H on the vegetable crops, and microclimate change (Cleugh leeward zone or between 0 and 3 H on the windward 1998) due windbreak effect. Temperature and evap- side (Baldwin 1988; Cleugh et al. 2002; Helmers and otranspiration rate have a positive influence over Brandle 2005). This research agrees with Helmers and plants behind the windbreaks, suffering less moisture Brandle (2005), demonstrating the yield response for a stress and leading to better growth due to less mid-day 123 Agroforest Syst Fig. 1 Crop yield response for a field windbreak. Modified from Read (1964) and Helmers and Brandle (2005) wilting and stomatal closure resulting in cessation of Willow (2) and Knox (1) counties. Fields were the photosynthetic activity (Andrue et al. 2009). The selected under the following criteria: long enough increase or decrease of evaporation rates depends on fields (length more than 30 times the height (H) of the weather, soil conditions, and plant water status windbreak) or pairs of fields, one with a windbreak and (Cleugh 1998). the other without in order to compare the yield in the To our knowledge, there are very few recent studies protected and un-protected zones. Only about 15% of evaluating crop yield benefits of windbreaks. Addi- the fields had the ideal adjacent protected and non- tionally, most of the studies (Bates 1944; Stoeckeler protected fields for comparison. The rest of the fields 1962; Brandle et al. 1984) have used small plots or had to use as unprotected control areas more than 30 H trials protected by windbreaks on research areas to downwind. record data, thus there can be issues of scale, Selected fields had windbreaks with good structural comparing plot yields to entire fields. A small pilot features: height (H), orientation, length, width, uni- study utilizing combine yield monitor data was formity, and continuity according to literature guide- conducted in Minnesota (Wyatt 2008). However, no lines (Brandle et al. 2000; Bates 1944). It is important reports could be found of geo-referenced crop yield to mention that most of the selected fields were long, monitor data being used in a windbreak study of this with more than 80 H length in units of windbreak scale. height. In those fields, the unprotected control area The main objective of this study was to develop a was considered starting at 30 H downwind, and this GIS approach using georeferenced combine-generated zone averaged more than two times larger than the crop yield monitoring data to: (1) determine if area of the windbreak protected area (20 H) in this windbreaks provide yield benefits for soybeans and study.
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