Management Options for Organic Winter Wheat Production under Climate Change

Farmers today face the challenge of adapting their crop cultivation methods to climatic changes. In the near future, farms with a high adaptive capacity will have a distinct advantage. The adaptive capacity of a farm is established first and foremost by expanding diversity and flexibility [1]. Between 2009 and 2014, strategies to increase the adaptive capacity of organic farms were developed within the interdisciplinary project Innovation Network of Climate Change Adaptation Brandenburg Berlin (INKA BB; http://www.inka-bb.de/). Addressing practical issues regarding climate change adaptation, farmers and scientists worked together to develop modification measures, which were then tested on-site [2]. This paper illustrates a farming system experiment probing test methods for adapting winter wheat cultivation to climate change. The experiment was carried out from 2010 to 2013 in northeast Germany on the stockless organic farm Wilmersdorf.

Winter wheat provides the economic foundation for the Wilmersdorf organic farm and has, thus far, been cultivated solely according to standard procedures. These standard organic farming procedures entail sowing winter wheat on fields prepared with a two-year multispecies legume- grass (LGS), which is mulched two to four times a year and ploughed under in autumn of the second harvest year. Directly following this virgin tillage (i.e. ploughing the sward without prior shallow soil processing), winter wheat is sown in mid-October. The subsequent crop is usually winter rye. This standard cultivation practice is practiced on large, rolling fields averaging 40 hectares, interspersed with hills and hollows. Such small-scale heterogeneity with varying soil types (see Section 2.2), further complicates ploughing and seedbed preparation. Poor soil contact and uneven germination are common problems. Particularly during dry periods, a common occurrence at Wilmersdorf (Section 2.3), hilltops are low yield (problem) areas and ploughing the shallow topsoil there is limited. In contrast, the hollows are often waterlogged, particularly in spring and in years with heavy precipitation, which also severely limits ploughing. The farm manager reports an annual fluctuation in winter wheat yields, between 0.9–5.8 t ha⁻¹ (Ø 3.5 t ha⁻¹). Therefore, to attain high winter wheat yields with the standard practice, the nitro- gen (N) supply from LGS residuals and the N-up-take vital to winter wheat development must occur synchronously [3]. This process is closely linked to the water supply and the soil’s microbial activity, which could be strongly influenced by climate changes projected for Brandenburg [4]. Such climatic developments include frequent mild and wet winters, increasing spring and summer droughts, recurrent extreme weather events (heavy rainfall and drought), and a rise in the average annual temperature [5]. Figure 1 depicts projected climatic changes from 2062 to 2092, illustrating their effects on the Wilmersdorf organic farm.

In view of these projected climate changes, the current standard cultivation practice reveals several weaknesses:

LGS virgin tilling in mid-October, followed by a mild and rainy winter, may lead to N-mineralisation, nitrate leaching and erosion, as the low development of winter wheat mass is unable to take up sufficient nitrogen at this time [6]. On the other hand, increasing drought in early spring reduces microbial nitrogen release [7]. This can result in an N-deficiency during developmental phases, when winter wheat has high nitrogen requirements (Stem elongation; Zadoks scale 30–32) [8]. Furthermore, ploughing in autumn heightens erosion susceptibility and the risk of plough sole compression [9]. As a result, root depth and infiltration can be retarded, hindering the soil’s buffering capacity in extreme weather events (heavy rain and drought).

These issues are compounded by the influence dry periods and increased precipitation in late autumn and winter has on the number of suitable fieldwork days for ploughing and sowing. In the future, winter crop sowing conditions could deteriorate in direct proportion to the instability of appropriate fieldwork days [10].

Since LGS processes great quantities of water via transpiration, increasing temperatures can potentially lead to a water shortage in the soil, inhibiting subsequent crop growth [9]. Despite uncertainties in climate predictions, the above listed weaknesses illustrate how strongly climatic changes may influence growth, site and weather conditions, and so of course crop yields. The question is, which strategies and measures can minimise yield risk in future winter wheat cultivation on the Wilmersdorf organic farm?

The extent of climate risks can be offset by increasing diversification within an agricultural ecosystem. This means not only introducing a greater diversity in crops and varieties, but also more flexibility in cultivation and tillage methods [12, 13]. Such alternative tilling and/or seeding methods help farmers more effectively adapt to changing weather conditions, extending the number of available fieldwork days.

To date, the Wilmersdorf organic farm has used only one method for producing winter wheat.

This work is therefore dedicated to the following questions: In addition to the standard practice, which winter wheat cultivation methods are most effective in offsetting climate change influences? Which methods contribute most to diversification on a specific farm?

In collaboration, the Wilmersdorf farm manager and the INKA BB field trial project a) developed new cultivation techniques and, b) tested the viability of these methods as alter- natives to standard procedures. When evaluating various courses of action, i.e. cultivation methods, for their adapt- ability to uncertain climate change conditions, robustness is an important criterion [14]. Robustness is a system’s immunity to a wide range of influences [15]. In this case, the robustness of a new cultivation method is measured by its yield stability over a three-year period under varying field conditions. Hallmarks of these new cultivation methods are reduced tillage and alternative crop rotation. They should be able to improve the N and water supply to winter wheat. These alternative cultivation methods, (Figure 2), and the reduced tillage agricultural tool, the ring-cutter, will be described in detail.

A new agricultural tool, the ring-cutter, was used for the first time during the field tests in Brandenburg. This agricultural instrument has cutting rings running diagonally to the driving direction, allowing for an overall, non-turning, shallow tillage (see: http://www.heko-landmaschinen.de). The special ring-cutter construction is intended for soil processing when dryness or sogginess renders ploughing unsuitable. As opposed to the plough, the ring-cutter could be applied to both the dry hilltops and damp hollows on Wilmersdorf farm. The tool should also enable unploughed LGS processing, so that grain mulch seeding (early sowing and oat/ring-cutter test methods) or catch crops can be seeded directly following ring-cutter processing. If ring-cutter processing proves successful, summer crops and early sowing can stay on schedule, despite wet or dry soil. At the same time, shallow processing can reduce the water loss caused by evaporation in ploughed soil. Reduced tillage with the ring-cutter should also retard N-mineralisation, reducing the risk of N-leaching in winter (see test method oat/ring-cutter) [16].

In the cultivation methods early sowing and catch crop, the LGS processing date is moved forward to mid-July (summer processing). This early treatment of LGS can either move winter wheat seeding forward or prepare a better seedbed than virgin tillage and an autumn furrow do. Instead of the plough, the ring-cutter is used for early, mechanical LGS killing. The early sowing test method repeats ring-cutter processing two or three times between mid-July and mid-August, creating a mulched summer fallow. This fallow protects the soil from water loss that would otherwise occur in living LGS crop transpiration [9]. The mulch also protects from evaporation, reducing water loss from the soil surface (evaporation fallow) [17], while seasonal heavy rains are buffered by the mulch (erosion protection) [18]. At the end of August, the catch crop mixture (50% summer vetch, Vicia sativa; 28% buckwheat, Fagopyrum esculentum; 16% flax, Linum usitatissimum; and 5% Phacelia) is sown directly into the summer fallow (mulch seeding). Not turning the earth protects soil life, keeping vertical earthworm channels (macropores) intact and improving infiltration [19–21]. Since it has a longer and stronger plant growth until its dormant season, early sown winter wheat should better absorb the nitrogen mineralised from late summer to early autumn [22, 23]. The catch crop mixture should suppress weed growth and prevent an overly lush development of the early sown winter wheat [24]. Furthermore, in autumn the catch crop absorbs any potential nitrogen surplus, conserving it in its biomass throughout the winter. In spring, the frozen catch crop vegetal material mineralizes the soil, supplying the winter wheat with the required nitrogen. Early sown winter wheat develops more profusely in spring, creating better rooting in the subsoil. This is conducive to the nitro- gen and water supply in the event of a spring drought. Also, early sowing pre-dates winter wheat primary water needs (stem elongation) to a time when the soil should still have enough winter moisture. Furthermore, the early seeding head-start in growth should assure the plants are no longer subjected to drought stress during the grain filling phase [25, 26]. The unploughed early sowing test method should primarily improve crop establishment and the subsequent grain yield on dry hilltops.

In contrast to early sowing, the catch crop test method does not have summer fallow. Instead, after repeated processing with the ring-cutter, the same catch crop mixture as in early sowing is sown at the end of July. The aim of the catch crop is to bind nitrogen mobilised by the early LGS tilling in summer, and to convert it into organic material which will have a narrow C/N ratio the following spring [27]. This material activates soil life, improving N resources for winter wheat. Coinciding with the standard autumn furrow, the catch crop is ploughed immediately before winter wheat late seeding (mid-October).

In the oat/plough and oat/ring-cutter test methods, LGS tillage takes place in late March. The advantage of spring-time tillage over autumn tillage is that the pre-winter mineralisation from LGS residuals, and so nitrate leaching, is nearly non-existent [6]. Compared to autumn tillage, spring tillage usually allows for a better balance between the N release from LGS residuals and N crop up-take [27]. Due to the generally cooler temperatures and a high C/N LGS residual ratio, tillage in spring can also go hand in hand with delayed N mineralisation [6, 27]. Since the mineralisation process following spring tillage begins later and lasts longer, often only the second subsequent crop profits from the N provided by multi-annual LGS [6]. For this reason, the oat/plough and oat/ring-cutter test methods switch crop rotation, growing oats prior to winter wheat. By inserting oats, the N-deployment from organic plant matter (decom- posed LGS residuals, straw and oat root residues) is more in sync with winter wheat N up-take the following spring. The advantages of oat as an LGS subsequent crop are its extensive root system and high nutrient up-take [28], while as a winter wheat preceding crop, oat’s vegetative growth suppresses weeds. As a recovery crop, oat prevents the spreading of fungal pathogens, such as black root rot (Gaeumannomyces graminis) [29, 30]. At the same time, the increased winter moisture resulting from climate change should be used productively for early oat cultivation, extending the cultivation period in the future. An earlier vegetation period grants a surplus of available fieldwork days for seeding spring grains [10, 31].

To keep future seeding on schedule despite higher winter precipitation (see Figure 1) saturating the soil, the oat/ring cutter test method foregoes ploughing, working the oats with the ring-cutter to establish mulch-till. After harvesting the oats, the stubble is worked with the ring-cutter. The oat straw remains on the field, as its broad C/N ratio helps prevent excessive LGS-residue N release in autumn and subsequent nitrate leaching in winter. In contrast to standard procedure virgin tillage, prior oat cultivation improves the winter wheat seedbed preparation and allows for a more flexible seeding schedule. In both oat test methods, winter wheat is sown at the end of September. In test method oat/ring-cutter, seeding follows reworking the soil with the ring-cutter— unploughed mulch-till—while test method oat/plough entails renewed ploughing. All unploughed test methods are designed to improve dry hilltop yields.

The robustness of each cultivation method is tested based on the following hypotheses:

(1) The ring-cutter effectively cuts and regulates LGS in both damp and dry soil conditions, where ploughing is restricted.

(2) Compared to the standard practice, winter wheat test methods ploughed in autumn, catch crop and oat/plough, produce equivalent annual grain yields, on hilltops as well as in hollows.

(3) The unploughed winter wheat test methods early sowing and oat/ring-cutter are particularly suitable for dry hilltop sites, where, when compared to hollows, the annual grain yields of these test methods come closer to those of standard practices.

The stockless organic farm Wilmersdorf (Bioland growers’ association member) is located in the north German low- lands in the northeast of Brandenburg (Uckermark; community Angermünde, district of Wilmersdorf: 53.11431^◦ N; 13.90660^◦ E). The farm has over 1,108 hectares of arable land and 5 hectares of grassland. Almost half of the arable land is used to grow legumes. Forage legume cultivation accounts for the main area (surface area 29%), followed by grain legume cultivation (19%). The remaining half of the arable land is reserved for growing grains, winter rye (28%) and winter wheat (20%), spelt (16%) and spring wheat (15%), as well as winter and spring barley (12% and 9%, respectively). Wilmersdorf has predominately sandy loamy soil and implements the following crop rotation: Alfalfa clover-grass / winter wheat / winter rye / field peas / spelt under sown with alfalfa clover-grass.

Wilmersdorf, located in the upper moraine region, is dominated by a hilly to undulating landscape of hills and hollows (40 to 75 meters above sea level) [32]. Sub-glacial till, lime-free loam or loamy sand prevail [32]. The topsoil is characterised by soil erosion and a low decalcification depth. Predominant is calcite luvisol/gley luvisol (brown soil family), known for both its fertility and its tendency to compress the topsoil foundation [32]. Typical, indigenous catena sequences are, from the hilltop to hollow, calcarite regosol > eroded calcite luvisol > gley luvisol > eutric gley [33]. In dry years, exposed hilltops are prone to yield reductions, while in wet years the loss occurs on the lower slopes and in the hollows [32]. At the same time, the eroded peaks exhibit higher pH values than the hollow depressions (Table 1).

Sandy loam was the predominant soil type in all sub-plots of the pilot facility. Considering a main root zone of 100 mm, sandy loam has a field capacity of 110 mm. In contrast to the hollows, the hilltops are carbonaceous, and average a higher proportion of clay and higher pH values (Table 1). The carbonate level indicates the initial till substrate which topsoil erosion has brought close to the surface. Soil samples found compressed topsoil foundation (soil depth 20–25 cm) on the shallow calcarite regosol hilltops (Ah/C soil). In the samples taken in 2011, the above-mentioned soil conditions were particularly pronounced. Ploughing was limited on the hilltops due to the shallow topsoil and the initial substrate’s proximity to the surface.

The Wilmersdorf climate is characterised by low annual rainfall and frequent dry periods in early summer and autumn. With 517 mm annual rainfall and an average annual temperature of 8.8^◦ C, it is one of the driest regions in Germany [32]. The three experiment years (2010–2013) were partially influenced by extreme weather patterns and high annual precipitation that exceeded the long-term average in all three years (Figure 3).

In 2010, high precipitation in summer (August: 117 mm; annual rainfall: 640 mm), made most fields impassable during both harvest and autumn sowing. 2011 was marked by a very warm and dry April and heavy rains in July (203 mm). Annual rainfall was 693 mm. Winter 2012 brought black frost and a succession of frost/thaw cycles, leading to considerable winterkill. The early sowing test method plots were so badly damaged by winterkill that they had to be reestablished with spring wheat. After a warm and a partially dry spring, above average precipitation fell in July (annual rainfall 626 mm). A prolonged and snowy 2012/2013 winter was followed by a pre-summer drought in April, then a dry and warm July and August. With an annual rainfall of 583 mm, 2013 was the driest project year.

The field trial was designed as a three-year serial experiment. Complying with crop rotation, the experiments were carried out on a different field each year. Two homogeneous fields (one hilltop, one hollow) were selected on each of these fields by interfacing digital plot, soil and yield maps. The trial cultivation systems were set upon the two sites in fully randomised blocks. Each block contained four plots divided into five sub-plots (20 sub-plots per site/40 sub-plots total). Except for reaping, the 15 m long by 5 m wide plots were worked with the customary combine harvester. The individual steps, deadlines and applied techniques are listed in Table 2. The selected ring-cutter tool had a three-meter working width, six cutting rings and a leaf spring roller for reconsolidating the soil. After the winter wheat harvest, the trial plots were completely ploughed and winter rye was cultivated.

The yields of oat, winter wheat, and subsequent winter rye (2012 and 2013) were assessed by documenting the number of ears per square meter, the thousand kernel weight and the grain yield. The crude protein content in winter wheat, an indication of grain quality, was measured as well as the oat hectolitre weight. The development and structure of crops were determined by visually appraising cultivated plants, weeds and catch crop mixture coverage [34]. Weed appraisal focused on pre-eminent weeds displaying a high degree of both consistency and coverage. Biomass growth was compiled by taking manual cuts (0.5 m2) from LGS, the oat crop and the summer catch crop. Depending on the test method (Figure 2), two manual LGS cuts were taken from plots of the early sowing and the catch crop method, and three cuts were taken from standard practice plots. All LGS cuts were taken independently, either before the usual mulching dates or prior to using the ring-cutter for the first time, respectively (Table 2). The LGS cuts from oat fields (Zadok scale 69) and from the summer catch crop were taken after buckwheat bloom [8]. To determine the respective yield share, the LGS and oats samples were sorted by hand. The N-input of the second harvest year was determined by calculating LGS biomass yield, leguminosae and N-content. With the N-balance calculator the N-input count was taken from N2-fusion minus gaseous N-losses that arise from mulching [35]. Soil samples to determine Nmincontent were extracted as weather conditions allowed (Pürkhauer drills, soil layer 0-60 cm), i.e. in autumn after winter wheat seeding, at the beginning of vegetation in spring and after the winter wheat harvest. For the extraction of the soil mineral nitrogen, $\mathrm{NH}_4-\mathrm{N}$ and $\mathrm{NO}_3-\mathrm{N} 2 \mathrm{M} \mathrm{KCl}$ solution was used. In 2010, due to drought, one shallower sample $(0-30 \mathrm{~cm}$ soil layer) was taken after the oat harvest in late summer. The statistical variance analysis was carried out with MIXED procedure (SAS 9.1 statistical software) and subsequently compared to the mean values (Tukey HSD test).

In accordance with test method design, the same LGS seed mix was sown on all plots over all three years. Over all three years, no substantial differences in the quantity of biomass growth on hilltops and hollows could be discovered (Table 3). However, there was a great difference in growth quality regarding which species grew on which site. On the hilltops, LGS growth regularly exhibited a higher percentage of alfalfa; in the hollows, more grasses, herbs, white clover and weeds (Table 4).

In 2010 and 2011 until mid-October, catch crop test plots achieved growth between 2.5 and 3.9 t DM ha⁻¹, (N up-take from 72 to 100 kg N ha⁻¹). In contrast, in 2012, low rainfall in August and unevenly distributed precipitation in September, caused summer catch crop plots to fail (Table 3).

In 2010 and 2012, oat yields were 21% and 54% higher in the oat/plough test method than in the oat/ring-cutter test method, respectively (Table 5). In each trial year, the yield difference between the two test methods was more pronounced in the hollows than on the peaks. Only on the hilltops in 2011, where ploughing was limited, (see Section 2.2), did the unploughed oat ring-cutter method achieve a 17% higher oat grain yield.

Among test methods, the winter wheat grain harvest varied considerably. This variance was most pronounced in the years with extreme weather conditions (2011 and 2012; see Section 2.3.).

In 2011 and 2012, winter wheat on the oat/plough and oat-ring-cutter test plots could not be harvested due to frequent heavy precipitation and a rampant weed infestation (Tripleurospermum perforatum). In all years and on all test plots, when harvesting was possible, winter wheat grown with the oat/ring-cutter test method produced the lowest grain yield of all test methods—significantly lower on hilltops in 2012 and 2013; and in hollows in 2013 (Table 6). In addition, the hilltop winter wheat in oat/ring-cutter test methods exhibited decidedly lower crude protein in 2011 and 2012. There was no great difference in grain yields between the standard procedure and early sowing and catch crop test methods. Compared to standard practices, however, the early sowing method had consistently lower grain yields. In 2011, the crude protein content in early sowing was markedly lower than in standard and catch crop methods. In contrast, in the dry year, 2013, early sowing exhibited a much higher thousand kernel weight than standard and catch crop methods. The catch crop method came closest to matching the standard practice in yield and quality. With the exception of catch crop in 2013, none of the alternative test methods were able to achieve a higher yield than the standard practice.

In 2012 and 2013, winter rye was a subsequent crop to winter wheat, bringing in high grain yields, especially in the hollows. With the exception of the thousand kernel weight in the hollows in 2013 there was no discernible difference between the test methods (Table 7).

The N-dynamic in cultivation methods was estimated based and catch crop wheat plots, which had been ploughed at a later date. Compared to the standard practice, oat/ring- cutter and oat/plough methods had significantly lower N_min- values in the spring (Hollow 2011–2013). There were no remarkable differences in N_min-values in samples taken from beneath the subsequent winter rye crop (08.11.2011, 22.10.2012), or taken immediately after the winter wheat harvest (08.02.2013; Table 11). The five highest N_min- values of all sampling dates were found in the subsequent winter rye crop (max. value, 148 kg Nha⁻¹; oat/ring-cutter test method).

Weed distribution varied on the different sites and test method plots. In all experimental years, the weed population in oats and winter wheat was more pronounced in the hollows than on the hilltops.

On average, the standard practice and catch crop test method (autumn ploughing and late seeding) had the lowest weed dockage, the weed coverage ratio (WCR) in both methods being nearly identical. In comparison, the early sowing WCR was from distinctly to significantly higher in each year. On the oat/ring-cutter plots there was usually a higher WCR (Table 12) and/or a higher weed biomass (Table 13) in established oat and winter wheat cultures than on the oat/plough (Op) test plots. In addition to these quantitative differences, specific differences were found in weed group composition on the varying sites and in the varying test methods.

The prior LGS crops generated weed flora—alfalfa (Medicago sativa L.), red and white clover (Trifolium repens L. and Trifolium pratense L.) as well as perennial ryegrass (Lolium perenne L.) and couch grass (Agropyron repens L.)—on all locations and test methods. Comparing stan- dard practices and ploughed test methods (catch crop, oat/plough) to the unploughed test methods (early sowing and oat/ring-cutter) (Table 13), alfalfa did not regrow in ploughed methods, neither in the preceding oat crop nor or in winter wheat. In 2011, however, alfalfa did re- grow on standard practices and catch crop hilltop plots because the plough could not optimally turn the soil in autumn. Besides alfalfa, the weed population was dominated by, in descending order, creeping thistle (Cirsium arvense L.), scentless chamomile (Tripleurospermum perforatum), poppy (Papaver rhoeas L.), common chickweed (Stellaria media L.), larkspur (Consolida regalis Gray) and veronica (Veronica chamaedrys L.). These species varied within sites and procedures. In the hollows and in the unploughed test methods, creeping thistle was much more dominant (Table 14), particularly in the oat/ring-cutter winter wheat. In the hollows and on one hilltop, scentless chamomile dominated, mainly in the early sowing, oat/ring-cutter and oat/plough winter wheat test methods (cover ratio, 75–90%). In 2011 and 2012, a rampant odourless chamomile infestation caused winter wheat crop failure in oat/plough and oat/ring-cutter hollows.

The experimental cultivation methods were carried out from 2010 to 2013 and were at times subject to extreme weather conditions. Only 2013 came close to long-term averages and predicted climate changes, such as pre-summer drought (see Figure 3). With this in mind, the following discussion addresses the extent to which the tests provide a practical alternative to standard practices and if they can contribute to diversifying winter wheat cultivation.

The hypothesis that the ring-cutter can effectively kill and regulate LGS in both wet (spring) and dry (summer) soils was confirmed—LGS secondary growth coverage on unploughed oat and wheat plots was the same height as on ploughed plots. The tool’s cutting technique - a shallow, vertical undercutting of the upper topsoil - separates the alfalfa sprout shaft below the root crowns, effectively impeding re-growth. In contrast to the plough, ring-cutter tractive power requirements are low and operating speed (11 km h⁻¹) is remarkably fast. Nonetheless, the tool required two to four working cycles to prepare the plots for mulch seeding after the two-year LGS cultivation. Further drawbacks to the ring-cutter were much lower grain yields in two of the three years on oat/ring-cutter and winter wheat plots and less N-availability than oat/plough plots. Ring-cutter implementation only reached higher oat yields than oat/plough on the shallow hilltop in the 2011 test method. Numerous other studies substantiate that reduced tillage in organic farming results in lower yields and lower N-availability [19, 36–39]. Reduced tillage limits N-availability by delaying soil organic matter (SOM) mineralisation, due to minimal aeration [19] and poor soil warming in the spring, particularly when densely mulched [40]. Especially in spring, unprocessed earth is often cooler and soggier than ploughed soil, hindering both germination and the initial growth of summer grains [41]. Reduced soil processing can also lead to increased compression in untreated layers [18, 39] and to accumulated SOM in the upper soil layer [42], as confirmed by ring-cutter processing research conducted at the ZALF Mu¨ ncheberg experimental station where much higher soil compression limited root penetration of winter grains [43]. Limited N, compressed soil and thwarted root growth impede a plant’s ability to absorb nutrients, which may have caused the much lower oat and winter wheat harvests [37]. In addition to these factors, the ring-cutter plots displayed dense weed growth (Tables 12 and 13); typ- ical for reduced tillage in organic farming [19, 44]. Shallow ring-cutter processing causes weed seeds to remain close to the surface, providing excellent germination conditions. Perennial species such as couch grass and creeping thistle thrive under reduced tillage [45].

Bearing all this in mind, it becomes clear that the results of reduced tillage are highly dependent on the time of ring-cutter processing, on crop rotation selection and on weather conditions, as confirmed by the completely unploughed oat/ring-cutter and early sowing test methods [18]. While oat/ring-cutter did not generate stable oats or winter wheat grain yields, the early sowing wheat yields of two trial years did not deviate greatly from standard procedure yields. Hence, reduced soil processing can be successful when applied to pertinent sites and adapted to the entire cultivation system, i.e. alterations in crop rotation, seeding and the catch crop [19].