1. Introduction
The world’s human population is predicted to reach 9.15 billion people by 2050, with demand for ruminant livestock products estimated to increase by between 1.4 and 1.8 the times 2010 consumption levels during this period [
1]. Meeting this demand will require additional feed resources, principally high quality forage, to overcome livestock production constraints caused by periods of deficit in both forage availability and/or forage quality [
2,
3,
4,
5]. Countries such as Australia, which is a major exporter of beef and sheepmeat, will seek to adapt their farming systems to sustainably increase production to meet this increased demand. These future ruminant livestock production systems will be shaped by world demand, seasonality of forage production, and the impacts of climate change.
In southern Australia, peak crop and pasture growth occur during the spring when both temperature and available soil moisture are favorable, with deficits in quality and availability occurring in summer and winter, respectively [
6,
7]. Climate change is predicted to exacerbate deficiencies in forage availability as seasons become drier and rainfall more variable [
4,
7]. Conservation of surplus pasture or specially grown crops as hay or silage is a management strategy that can be used to fill seasonal feed gaps and increase production [
8]. In addition, conserved forage can be used to minimize risk, manage climate change, reduce the impact of floods and drought, and maintain productive capacity of the breeding herd from year to year through access to an additional source of stored fodder.
Production systems that use conserved forage can be used to redistribute forage grown across a year and to remove grazing pressure on pasture during periods of low availability. Consequently, removing the risk of overgrazing can lead to adverse effects on soil and other plant species, particularly under adverse climatic events, such as drought. A well-managed forage conservation program will utilize plant species that most appropriately match climatic and soil physicochemical constraints and also maintain or improve the natural resource base [
7]. These species will require attributes of adaptation to variable climatic conditions with capacity to produce harvestable quantities of material of high nutritive value to optimize livestock production, even under moisture-constrained conditions.
Cereals (wheat, barley, triticale, oats) are ideally suited to southern Australia, producing good yields of forage for conservation under a range of seasonal conditions [
9,
10]. However, cereal crops often have low to moderate protein levels when conserved, making them less than ideal for highly productive livestock, including dairy cows, young growing sheep, and cattle [
10,
11,
12,
13]. Legumes such as field pea (
Pisum sativum L.) and vetch (
Vicia spp.) have higher protein and digestibility but can be lower yielding and require physical support to prevent lodging [
14]. Growing cereals in mixtures with one of these legumes is an option to increase yield, reduce lodging, and produce forage with adequate energy and protein levels [
15,
16,
17]. Growing legumes in mixtures with cereals also removes the need to supply fertilizer nitrogen (N) to the crop [
18].
Several authors have reported the benefits of cereal–legume forage crops, such as those indicated previously. This has included studies from a number of countries and regions including the United Kingdom, Europe, North America, and Western Asia [
18,
19,
20,
21]. The locations include a diversity of soil types, cereal and legume species and varieties, rainfall (and irrigation), and fertilizer, as well as a range of measured crop yield and quality attributes. The diversity in yield and quality highlights the need for regional research and helps to identify the best combinations for local conditions. Furthermore, while some studies reported the effect of varying the ratio of legume to cereal seed at sowing on yield and quality for vetch, pea, wheat, barley, oat, and triticale combinations [
18,
19,
22,
23,
24], those specifically comparing triticale to pea ratios are much less [
25]. These studies did not examine the effect of varying the cereal and legume component sowing rates independently of each other, and most were restricted to only one or two harvest times, i.e., stages of plant maturity.
In Australia, there are limited data on the management of cereal–legume mixtures for hay and silage production. Thus, there are questions around what the optimum sowing rates, harvest times, preferred species, types, and varieties are [
13]. This paper reports on the agronomic and feed quality attributes of triticale–pea forages grown to test the hypotheses that (1) a higher pea–triticale content leads to increased forage feed value; (2) forage quality declines with increasing plant maturity; and, (3) forage type field peas have higher quality than a semi-leafless variety.
3. Results
The yield varied between years (
p < 0.05) such that 2010 > 2011 > 2009 for all triticale and pea sowing rates and individual harvests, consistent with differences in rainfall received. There were interactions between year and triticale sowing rate (
p = 0.031), year and pea sowing rate (
p = 0.007), and year and harvest (
p < 0.001) (
Table 2). The yield was higher (
p < 0.05) for T15 compared to T30 and T45, and for P80 compared to P40 in 2010. The yield increased (
p < 0.05) with successive harvests (triticale maturity) in each year except between H2 and H3 in 2011. The interaction between the triticale and pea sowing rate (
p = 0.019) was also significant. The yields were higher (
p < 0.05) for P80 compared to P40 at T15 (14,659 vs. 13,120 kg DM/ha) and T30 (14,833 vs. 12,992 kg DM/ha) but not T45 (13,900 vs. 14,030 kg DM/ha).
The crop dry matter content varied due to the interaction between the triticale sowing rate, harvest, and year (
p = 0.005) (
Table 3). The dry matter content at the boot stage was lower (
p < 0.05) in 2009 and 2010 compared to 2011, and similar to the flower stage harvest in 2010. The dry matter content increased (
p < 0.05) with successive harvests and varied (
p < 0.05) with the triticale sowing rate at the final harvest in all years.
The crop pea content varied with the interaction between year and pea variety (
p = 0.003), as the pea content was higher (
p < 0.05) for Morgan than Parafield in 2009 and 2011, while the proportion of pea in the Parafield crops was higher (
p < 0.05) in 2010 compared to 2009 and 2011 (
Table 4).
The pea content also varied with triticale by the pea sowing rate interaction (
p = 0.044). The pea content was highest (
p < 0.05) at T15-P80 and higher (
p < 0.05) for P80 than P40 in combination with T15 and T30 but not T45 (
Table 5). The pea content declined (
p < 0.05) as the triticale sowing rate increased so that T15 > T30 and T45 at P40 and T15 > T30 > T45 at P80.
The crop digestibility varied with interactions between pea variety and pea sowing rate (
p = 0.038), and pea variety and triticale maturity at harvest (
p = 0.038) (
Table 6). The crops containing Parafield had higher digestibility (
p < 0.05) than those containing Morgan at P80. The digestibility was highest (
p > 0.05) in crops containing Parafield at H1, and higher (
p > 0.05) than Morgan at H1 and H3. Crops with the lowest digestibility were those containing Morgan harvested at H2 and H3 and Parafield at H2.
The crude protein content varied with the main effects of harvest (
p < 0.001, l.s.d
(p < 0.005) = 4.44) and pea variety (
p = 0.007, l.s.d
(p < 0.005) = 3.48), and the interaction between triticale and pea sowing rates (
p = 0.005) (
Table 7). The crude protein content declined (
p < 0.05) with each successive harvest to be 139.6, 117.4, and 102.0 g kg
−1 DM at H1, H2, and H3, respectively. Though the difference was small, the CP content of crops containing Morgan (122.1 g kg
−1 DM) was higher (
p < 0.05) than those containing Parafield (117.3 g kg
−1 DM). The crude protein content was higher (
p < 0.05) for P80 compared to P40 for T15 and T30 crops, while the CP content of P80 crops declined (
p < 0.05) with the triticale sowing rate, such that T15 > T30 > T45.
Differences in the WSC content between treatments was small, but the main effects of the pea sowing rate (p = 0.014, l.s.d(p < 0.005) = 6.19), pea variety (p < 0.001, l.s.d(p < 0.005) = 6.07), and harvest (p = 0.009, l.s.d(p < 0.005) = 8.12) were all significant. The water-soluble carbohydrate content was higher (p < 0.05) for P40 than P80 (163.2 vs. 155.9 g kg−1 DM); was higher (p < 0.05) for Parafield than Morgan crops (166.6 vs. 152.4 g kg−1 DM); and declined (p < 0.05) with harvest so that H1 (166.4 g kg−1 DM) was higher (p < 0.05) than H3 (153.6 g kg−1 DM), while H2 (158.5 g kg−1 DM) was intermediate and not different to either.
Significant differences in the ADF content occurred due to the triticale sowing rate (
p < 0.001), harvest (
p < 0.001), and the interaction between the pea sowing rate and pea variety (
p = 0.009) (
Table 8). There were also significant differences in the NDF content due to harvest (
p < 0.001) and the interaction between the triticale sowing rate and the pea sowing rate (
p = 0.043) (
Table 8). The acid detergent fiber content was lower (
p < 0.05) for T15 (281.0 g kg
−1 DM) compared to T30 (288.8 g kg
−1 DM) and T45 (292.0 g kg
−1 DM), and varied (
p < 0.05) such that H3 (264.4 g kg
−1 DM) < H1 (287.5 g kg
−1 DM) < H2 (309.7 g kg
−1 DM). Similarly, NDF also varied (
p < 0.05), such that H3 (451.4 g kg
−1 DM) < H1 (480.7 g kg
−1 DM) < H2 (510.1 g kg
−1 DM). The ADF content of the P80 Parafield crops was lower (
p < 0.05) than either the P40 Parafield or both P40 and P80 Morgan crops. The lowest (
p < 0.05) NDF content occurred when the highest rate of pea was sown with the lowest rate of triticale; in contrast, the highest (
p < 0.05) NDF occurred when the lowest rate of pea was sown with the highest rate of triticale. Within the pea sowing rate, the NDF content increased (
p < 0.05) between T15 and T45.
4. Discussion
These experiments were conducted to test the hypotheses that (1) a higher pea–triticale content leads to increased forage feed value; (2) forage quality of triticale–pea crops declines with increasing plant maturity; and (3) forage-type peas have higher quality than a semi-leafless variety. We can report that the DOMD and CP content of the crops in these experiments was within the range reported for similar crops in Australia and overseas [
10,
25,
33,
34], and could therefore be considered typical. We concluded that our results do not support the first hypothesis, and that a higher pea–triticale content leads to increased forage value. A higher pea content did not increase digestibility, and, though CP content was higher for P80 than P40 crops when sown at T15 and T30, the impact of this additional CP on liveweight gain was predicted to be only minor. For example, the increase in liveweight gain by young growing castrate male lambs fed these crops as the sole diet was estimated to be <2% [
35]. Furthermore, the additional gain would be restricted to crops harvested at the boot stage (H1) when DOMD was highest. This observation is consistent with Jacobs et al. who similarly reported that peas did not consistently and significantly improve nutritive value when grown in combination with triticale [
25].
Furthermore, our second hypothesis, that forage quality declined with maturity, as determined by digestibility and CP content, was proven true. The average digestibility and CP content declined by 68 and 37 g/kg, respectively, between the boot (H1) and milk stage (H3) harvests. The magnitude of this decline in digestibility and CP content was within the range previously reported for mixed cereal–legume crops grown across a range of environments [
10,
11,
14,
25,
33,
36].
Finally, we found the effect of pea variety on forage quality was equivocal and, there-fore, we consider our third hypothesis to be neither proven nor disproven. Despite the average pea content of Parafield crops being lower than Morgan crops (384.8 vs. 486.4 g/kg), the digestibility of Parafield crops was 21.2 g/kg higher than Morgan at the higher pea sowing rate. However, within a pea variety, the pea sowing rate did not affect digestibility. Furthermore, the digestibility of crops containing Parafield pea was 16.0 and 23.4 g/kg higher than those containing Morgan when harvested at the boot (H1) and milk (H3) stages of cereal development, respectively. This is possible due to a higher digestibility of, triticale, or both species compared to Morgan. However, the lack of difference between Parafield and Morgan crops at P40, when triticale represented a greater proportion of the crops, would favor the likelihood of higher Parafield digestibility. It would also require the Parafield digestibility advantage to be sufficiently large in order to counter the effect of reduced pea content of Parafield crops, indicating substantially higher digestibility than Morgan.
Interestingly, the digestibility of Parafield crops increased between H2 and H3. Previous research has indicated that cereal crops, including triticale, continue to decline after the boot stage up to and including the milk stage, equivalent to H1 and H3, respectively [
13,
36,
37,
38]. However, some crops can increase digestibility thereafter due to increasing starch accumulation [
39,
40]. A possible explanation based on our experiment is the increased pea content at H3 compared to H2; however, the proportion of pea did not differ between harvests and, therefore, we discount that possibility. Alternatively, the digestibility of the pea fraction may have increased during this period; however, this was not measured. An increase in the pea digestibility or the metabolisable energy (ME: MJ kg
−1 DM) content following an initial decline has been reported in some experiments, but not in others [
16,
25,
41]. It would also indicate a difference in the pattern of digestibility change between the two pea phenotypes. A search in the literature indicated limited data on digestibility changes for a range of pea types and varieties grown under the same conditions. More importantly, we were unable to find any published literature on changes in digestibility that compared a range of different pea types and varieties grown under the same conditions. Based on the apparent differences observed in this experiment, it is therefore recommended that future research should investigate the digestibility of different pea types and varieties at different stages of maturity to identify superior varieties.
The average CP content of crops containing Morgan was higher than those containing Parafield, but the difference was small (4.8 g/kg DM) and unlikely to be of any practical significance. Furthermore, considering that the Morgan pea content was, on average, 26% higher than Parafield, it is highly probable that the CP content of Parafield plants was higher than Morgan plants, but this was not measured. Given the trends in the pea content, DOMD and CP between the two crop types, a relatively higher sowing rate of pea and/or a lower rate of triticale for Parafield crops compared to Morgan crops has merit. However, further experimentation to compare crops with equal proportions of pea and for a range of pea types and varieties is required to confirm the biological and economic merit of this.
The content of water-soluble carbohydrates reflected the content of crop triticale, following treatments that increased the triticale content, i.e., using Parafield and a lower pea sowing rate, which increased WSC, though differences were small and would have no practical or biological significance either for livestock or during conservation. Similarly, a higher triticale content was associated with a higher NDF content, though differences were also small. However, the effect of higher triticale content on ADF content was equivocal, with reduced ADF on P80 compared to P40 crops, but no difference for Morgan. We speculate that the ADF content of Parafield was lower than both Morgan and triticale, which were likely similar, consistent with the fact that Parafield has higher digestibility.
Previous experiments have reported a diverse range in yields for similar forage crops from a range of environments [
12,
14,
36,
42,
43,
44,
45,
46,
47]. The yield difference between years in these experiments was substantial and reflected differences in the growing season rainfall between years [
19]. The yields achieved in 2010 were high but not inconsistent with other reports for forage and grain crops grown under ideal conditions in Australia or overseas [
13,
44,
48]. The yields were generally unaffected by both the triticale or pea sowing rate, which is consistent with a previous study [
49]. This indicates that plants are compensated by increased tillering and/or each plant growing when lower sowing rates are used. The exception was in 2010 when growing conditions were very favorable and highest yields were associated with the highest sowing rate of pea or the lowest sowing rate of triticale. We believe that these conditions allowed the pea to capitalize on their more indeterminate growth habit and continue to accumulate biomass for a prolonged period.
Different seasons also had a marked effect on the crop DM content at harvest. In addition to higher yields, higher growing season rainfall was associated with lower DM crops. These crops require more extensive wilting to reduce moisture content, but yield may reduce wilting rate because less forage is exposed to solar radiation. Consequently, with regards to higher yielding, low DM crops will have greater field and respiration losses during wilting, which will be exacerbated when conditions are less favorable, i.e., cool and overcast conditions. Slower drying rates also increase the risk of exposure to rain and greater losses. Conversely, lower growing season rainfall crops beneficially had a higher DM content, but exceeded the recommended level of 350 g/kg for chopped silage when harvested at the milk stage in 2011, making compaction more difficult. We observed that the variability in DM and yield has practical implications, as hay and silage help to manage crop production during wilting. With higher yielding, lower DM crops require more active intervention, including conditioning and tedding, in order to achieve a wilt within a short time period.
The yields exceeded that of a typical self-regenerating annual pasture, which is the most common pasture type in the region [
50]. These pastures are normally grazed but can be conserved as hay or silage. More importantly, liveweight gain is estimated to average 1148 kg ha
−1 (with a range of 443–2790 kg), if fed as the sole diet to 35 kg, six-month-old, crossbred (Border Leicester x Merino or Dorset x Merino) castrated male (wether) lambs [
35], assuming 70% utilization of the forage harvest. This favorably compares with lamb production from pasture (914 kg ha
−1: range 512–1315 kg ha
−1), allowing for higher pasture ME (12 vs. 11.7 MJ kg
−1 DM with no decline over time) than that observed for the best crops. Interestingly, despite an increase in yield with successive harvests, estimated lamb production per hectare remained essentially unchanged as the yield increase was offset by a reduction in ME after H1. The estimated lamb growth rates at H2 and H3 were 55.7% and 50.1% of H1, respectively [
35]. Lower harvesting, storage, and feedout costs, as well as slower lamb growth, indicate that harvesting at H1 is likely to be the optimum harvest time. This is consistent with recommendations for cereal and cereal–vetch crops grown in the same region [
14,
51].