3.2. Soil Properties
Physicochemical properties of soil at three soil depths before trial are included in
Table 2. Soils at the study site were sandy loam-loam (sand: 47.9 ± 2.42%; silt: 45.5 ± 2.31%; and clay: 6.6 ± 1.61%) and there were trends for proportions of sand decreased (
p = 0.10) and silt increased (
p = 0.09) at 15 to 60 cm depths. No treatment × depth interaction was observed (
p > 0.05) for all measured parameters. The electrical conductivity (EC; 6.74 ± 0.228 dS m
−1), organic carbon (OC; 1.2 ± 0.01% DM), and pH (7.62 ± 0.025) of the soils averaged among depths showed no differences across the treatment plots (
p > 0.05) prior to the initiation of the trial. While soil pH was uniform at the soil depths (7.62;
p = 0.45), a trend to slightly lower EC at 30–60 cm depth (6.39 ± 0.67 dS m
−1) (
p = 0.10) was observed. Soil salinity of EC > 4 dS m
−1 will restrict growth of many plants [
31], which suggests under the salinity level (ranged 5.9–7.1 dS m
−1) at the study site, plant growth, in general, will be detrimentally affected by the salinity depending on their salt tolerance level. Thus, as spring soil results indicate, soil at the trial site is considered a saline soil (EC > 4.0 dS m
−1 and pH < 8.5; [
32,
33] or according to the U.S. Salinity Laboratory classification [
34], fits in moderate (EC 4.0–8.0 dS m
−1) salinity interval. Soil levels of OC, available N, P, and K before trial, declined (
p < 0.01) as the soil depths increased, with the greatest amounts in 0–15 cm depth. Sulfate-S levels were in the very high range determined in a Saskatchewan study [
35] at all three soil depths because of the presence of sulfate salts associated with the salinity.
Physicochemical properties of soil at three soil depths after harvest averaged across the 3 years are included in
Table 3. Soil pH at the site in fall was 7.84 ± 0.044 with a trend of more alkaline (7.87 ± 0.044;
p = 0.073) condition at 15–30 cm soil depth, whereas the magnitude of EC differed (
p < 0.01), as before the trial, with lower EC (6.40 ± 0.182 dS m
−1) at 30–60 cm depth than either at 15–30 cm (7.31 ± 0.182 dS m
−1) or 0–15 cm (7.75 ± 0.182 dS m
−1).
Soil nitrate-N, phosphate-P, and K levels were lower or comparable when compared to the average surface soil N levels across Alberta, Saskatchewan, and Manitoba (9 kg ha
−1) [
36] and to the median amount of plant available inorganic N, P, and K (16, 17, and 671.3 kg ha
−1, respectively) in the top 45 cm of the dark brown soil of Saskatchewan [
35].
Overall, establishment and growth of the forage mixtures over the 2019–2021 period had relatively little effect on soil properties (
Table 2 and
Table 3), and no significant treatment effects were observed.
3.3. Stand Establishment, Botanical Composition, and Forage Yield of ‘Halo’ Alfalfa and Grass Mixtures
Evaluation of stand establishment of ‘Halo’ alfalfa and grass mixtures over two production years following the establishment year (2020, Yr 1, and 2021, Yr 2) is presented in
Figure 2. Stand success is most reliably assessed in the second or third growing season following establishment under non-irrigated conditions [
37].
Stand establishment of all mixtures were similar (p > 0.05) (avg. 81.7%) over the two production years, but the binary mixtures had a slightly better establishment (6.5% greater) than quaternary mixture (83.4 vs. 76.9%), especially in Yr 1 (10% greater). Quaternary mixture stands in Yr 2 showed greater (p = 0.01) establishment than in Yr 1 (85 vs. 68.8%).
Forage total dry matter yield (DMY) and botanical composition of the treatments are presented in
Table 4. Treatments did not differ (
p > 0.05) in total DMY over 2 yrs, but a trend (
p = 0.08) was observed for ALF-CMF of decreased total DMY in Yr 2 from Yr 1 (2.8 vs. 4.2 ± 0.46 Mg ha
−1). Forage mixtures in Yr 1 can be ranked according to mean yield as ALF-SWG the lowest yielding (3.2 ± 0.64 Mg ha
−1), ALF-SBG (3.5 ± 0.64 Mg ha
−1) and ALF- CMF-SBG-SWG (3.6 ± 0.64 Mg ha
−1) intermediate, and ALF-CMF (4.2 ± 0.64 Mg ha
−1) as highest yielding. Consistent with these results, at Swift Current, SK, in the semiarid region of the Canadian prairies, when Dahurian wildrye grass [
Elymus dahuricus Turcz. Ex Griseb], intermediate wheatgrass [
Elytrigia intermedia (Host) Nevski], and slender wheatgrass [
Elymus trachycaulus (Link.) Gould ex Shinners] were grown with alfalfa, the grasses produced similar forage yield and yield compensation by alfalfa grown with Dahurian wildrye and slender wheatgrass produced similar total forage yield [
38].
In comparison, the total DMY of ALF-CMF (4.2 Mg ha
–1), ALF-SWG (3.2 Mg ha
−1), and ALF-SBG (3.5 Mg ha
−1), in the current study, were lower than in a study conducted in Wyoming, USA [
15], with ‘Garrison’ creeping foxtail in mixture with alfalfa (10.1 Mg ha
−1), with ‘Lutana’ cicer milkvetch (6.5 Mg ha
−1), and with ‘Eski’ sainfoin (4.0 Mg ha
−1).
However, the total DMY of SWG in mixture with ‘Beaver’ alfalfa (3.5 Mg ha
−1) at Swift Current, SK, [
38] on a non-saline soil was comparable with the yields obtained in the current study, and those of ‘VNS’ smooth brome in mixture with ‘55V48′ alfalfa (5.1 Mg ha
−1) in North Dakota, USA, [
39] and of alfalfa + SBG mixture grown in the Mediterranean region of Turkey (2.6-3.3 Mg ha
−1) [
40] were higher and comparable, respectively.
Although there was no difference (p > 0.05) in forage component yield between treatments, the legume component, ‘Halo’ alfalfa mixed with CMF had numerically higher yield in Yr 1 (2.4 vs. 1.0–1.1 Mg ha−1 in other mixtures). However, this numerical difference was not observed in Yr 2 as legume yields in ALF-CMF (p = 0.02) and ALF-SBG (p = 0.01) were significantly lower, likely because of the dry conditions.
At Swift Current, SK, alfalfa (cv. ‘Beaver’) in mixture with SWG contributed 71 to 82% of the yield [
38], compared to which alfalfa, in the present study, made a lower contribution of 34% in Yr 1 and less, 27.6%, in Yr 2. This was not surprising as salt-tolerant grasses generally outperform legumes in moderate saline conditions. However, the legume percentages were still significant, close to the recommended level (30–40%) for grass–legume mixtures by Sanderson et al. [
41]. Studies in the northern Great Plains (North Dakota) have found SBG in the mixture with alfalfa made on average about 50% of the total biomass in the third production year [
42]. The yield of the grass component of first cut grass–‘Rangelander’ alfalfa mixtures averaged 33% of total yield for ‘Lincoln’ smooth bromegrass in the fifth production year [
43]. In comparison, SBG yield in the current study in Yr 1 (32.2% of total DMY) was lower or comparable, whereas, in Yr 2 (37.6% of total DMY) it was lower or higher, respectively.
Higher yields have been reported for these forages grown alone in saline conditions elsewhere. When grown on saline soil at Swift Current, SK, slender wheatgrass, smooth bromegrass, and creeping foxtail yielded 4.2, 5.7, and 5.4 Mg ha
−1, respectively, at seed set stage [
44]; ‘Radisson’ smooth bromegrass has produced 5.2 and 4.2 Mg ha
−1 at Saskatoon, SK, between 1982–1986 [
17]; and high total forage yields of 13.6 Mg ha
−1 and ranging from 24.2 to 32.7 t ha
−1 were achieved for alfalfa grown alone in saline-alkali soil regions of Turkey [
45] and north China [
46], respectively.
The results in the current study showed that the ALF-CMF binary mixture produced 9 to 23% greater DMY relative to the other three forage mixtures over two years on this moderate saline soil. Concurring with our findings, others noted good performance and salt-tolerance abilities of ‘Garrison’ creeping foxtail in North Dakota, USA, in soils of EC 6.5–7.0 dS m
−1 [
11], of ‘Halo’ alfalfa that produced a high relative shoot mass at 8 dS m
−1 [
47], and slender wheatgrass characterized as a salt-tolerant grass, able to withstand EC levels from 15–25 dS m
−1 [
11], or when combined together also appear to offer yield advantages over combination with a non-salt-tolerant grass like smooth bromegrass. In addition, ALF-SBG tended (
p = 0.09) to have more of the weeds, which possibly explains the legume decline as due to competition in these mixtures. Specifically, ALF-CMF was invaded 71.7% more with other weeds as compared to ALF-SWG (the least weed-infested) or to other mixtures (
p = 0.05). Slender wheatgrass tended to decrease (
p = 0.07) in yield in binary mixture with Halo alfalfa in Yr 2 by almost half (by 43.7%), indicative of possibly shorter longevity (short-lived vs. long-lived) and less persistence (moderate vs. high) [
48] of this grass species as compared to the other two grass species.
The results suggest that ‘Halo’ alfalfa with ‘Revenue’ SWG was less susceptible to weed invasion, whereas ‘Halo’ alfalfa with ‘Garrison’ CMF was more susceptible. In an Alberta, Canada site, where the salinity ranged from slight to moderate, green/slender wheatgrass mix and smooth bromegrass were among the forage treatments that successfully suppressed foxtail barley [
49]. Steppuhn et al. [
50] concluded that in controlling weeds that included foxtail barley, SWG grown alternating with green wheatgrass (
Elymus hoffmannii Jensen and Asay) was among the most effective treatments. However, a study with 11 grasses grown on a saline soil in southwestern Saskatchewan contradicted our findings in that slender wheatgrass (73% in botanical composition) appeared to be more susceptible to weeds than creeping foxtail (97% in botanical composition) or smooth bromegrass (91% in botanical composition) [
44]. It is speculated that because of the drought conditions experienced in the spring to summer of the establishment year (2019), the poor spring moisture may have affected the treatments the most with severe weed competition.
Likewise, studying the ability of forage crops to suppress weeds at mostly saline sites of Saskatchewan and Alberta, Canada, Steppuhn et al. [
51] observed that drought years seemed to favor foxtail barley growth at slightly to moderately and moderately to severely salinized sites. Wall and Steppuhn [
49] concluded that the more severe the salinity, the greater the challenge for the forage to suppress the weeds, the narrower the choice of forage species that will succeed, and the more favorable environmental conditions are needed. As well, identifying problems for salt-affected sites in the northern Great Plains, Tober et al. [
11] noted that the symptoms may include decreased crop yield and vigorous kochia or foxtail barley growth.
3.4. Forage Nutrient Composition, Yield, and Uptake
Forage mixtures did not differ (
p > 0.05) in nutrient composition (
Table 5). However, a trend (
p = 0.09) existed in ALF-SWG having greater TDN than the other mixtures in Yr 2. Forages with an RFV value over 151, between 150–125, 124–103, 102–87, 86–75, and less than 75 are categorized as prime, premium, good, fair, poor, and rejected, respectively [
52], based on which, forages in the present study (ranged 90.8–106.3) may be categorized as of good and fair quality.
Forage mixture treatments did not vary in the amounts of CP (CPY) and TDN (TDNY) obtainable from a hectare, nor between years; however, the quaternary mixture tended to decrease in CPY in Yr 2 (
p = 0.08) (
Table 6).
There was no difference between treatments in nutrient uptake or NUE (
p > 0.05) as shown in
Table 7. However, the year effect on nutrient uptake was significant (
p < 0.05) with decreased values in Yr 2 for some treatments, likely because of the drought condition experienced that year. Thus, in Yr 2, K uptake declined (22.7 vs. 45.3 kg ha
−1;
p = 0.02) in ALF-SWG and there were trends of lower P uptake (
p = 0.08) in ALF-SWG and ALF-CMF (
p = 0.10). As well, ALF-CMF and ALF-SBG appeared to have numerically higher K and N uptakes than the other mixtures.
Plants that are efficient in absorption and utilization of nutrients greatly enhance the efficiency of applied fertilizers, reducing cost of inputs, and preventing losses of nutrients to ecosystems [
53]. In terms of NUE, the mixtures ranged from 54.3 to 76.3 (
p > 0.05), but ALF-SWG appeared relatively more efficient than others (67.8 vs. 58.1 in Yr 1 and 76.3 vs. 63 in Yr 2) over two production years. In addition, NUE of the quaternary mixture was higher by 24.4% (71.5 vs. 57.5;
p = 0.11) in the second production year than in the previous year.
The NUE values of the mixtures grown on the saline soil, in the current study, were in the typical range of NUE (30–60) for cereals [
54], comparable to the NUE in maize (57) in the USA [
52], and greater than the average cereal NUE value (44) in the UK [
54], for annual wheat (38.3) [
55], and the worldwide NUE of approximately 33 percent for cereal production [
56].