1. Introduction
Soybean (
Glycine max L.) is the most important leguminous grain crop in the world. In an association with rhizobium bacteria, soybean fixes N
2 through biological nitrogen fixation (BNF). It is an important part of the human diet and contributes to livestock feed because of its high protein concentration [
1]. In addition, after grain harvest, crop residues supply nitrogen to subsequent crops and improve soil properties [
2].
Due to climate change and global warming, many areas where intensive soybean production occurs have experienced challenges associated with changing weather patterns and frequent occurrences of extreme weather events [
3,
4]. For example, soybean yield reduction has followed the occurrence of flooding during germination and early seedling growth [
5]. Waterlogging-restricted seed germination and initial root development damage the water and nutrient uptake capability of the crop [
5]. The scarcity of water negatively impacts the symbiotic association at its early stages by damaging the signal exchange between host plants and rhizobia. Thus, BNF by soybean was highly susceptible to drought [
6].
Crop rotation refers to the practice of cultivating various crops in sequence on the same field. Utilizing cover crops in a rotation may have several benefits that could ameliorate challenges associated with climate change, including increased soil fertility, reduced soil erosion, and enhanced soil moisture retention and weed suppression [
7,
8,
9,
10].
Italian ryegrass (
Lolium multiflorum, IRG) is a winter-annual forage and cover crop that can be rotated with summer crops. IRG is rotated with cotton and peanut in the southern United States, and it is currently widely grown as a winter forage crop in rice paddies during the winter season in Korea [
11]. If IRG is used for forage, growers can have an additional source of income. As a forage crop, above-ground biomass of IRG can be utilized for animal feed, while its roots and stubble residue can protect the soil. Previous studies have reported that IRG had a greater root biomass, root length, and root surface area than other cover crops, and that it continues to produce roots until late growth stages [
10,
12]. As a result, it can provide more below-ground biomass than other cover crops, and longer root persistence is associated with the provision of a greater amount of nutrients to the subsequent primary crop [
13]. As a cover crop, IRG increased soil organic carbon more than leguminous crops [
14]. Additionally, nine years of IRG use resulted in greater soil organic N accumulation than other green manure crops such as hairy vetch [
15]. When 40 Mg ha
−1 of IRG were incorporated as a green manure, it improved soil total N and available K, and increased seedling biomass of rice in an IRG–rice rotation [
16]. Although there are significant potential benefits of using IRG as a green manure, research is limited, especially regarding its effects on subsequent crops in the rotation. As a result, it is necessary to experiment with various crop rotations involving IRG, particularly to determine their impact on subsequent crops such as soybean. For instance, physiological and morphological responses of above- and below-ground parts of following soybean crop have not been tested in a multi-year field scale by different regimes of IRG usage.
Thus, the objectives of the current study were to determine: (1) The effects of incorporating IRG to existing soybean production as a novel rotational cropping system for the region; (2) The comparison of different usage regime and ecotypes of IRG on subsequent soybean shoot and root development; and (3) The evaluation of IRG biomass and nitrogen contents as a potential N supply to following soybean production.
3. Results
3.1. Soybean Yield Components and Grain Yield
Soybean yield components were compared for three years (
Table 4). The number of pods and grains did not differ between the treatments for three years of study. Across the treatments during 2020, the average number of grains tended to have lower values compared to those of 2021 and 2022. There were no significant differences between the treatments in 100-grain weight both in 2020 and 2021, while in 2022, a significant difference was observed (
p = 0.0163). In 2022, the Win+CC had the highest 100-grain weight value (31.4 g), while the Win−CC had the lowest value (27.8 g). The average 100-grain weight across the treatment was 26.0, 28.1, and 29.2 g in 2020, 2021, and 2022, respectively.
For soybean grain yield, there were no differences in 2020, but both 2021 and 2022 showed significant differences among treatments (
Table 4). In 2020, the average grain yield for +CC was 2.22 Mg ha
−1, while F yields were 1.83 Mg ha
−1. In 2021, the grain yield was greatest for Ko+CC (2.40 Mg ha
−1) and Win+CC (2.46 Mg ha
−1), while it was least for Win−CC (1.83 Mg ha
−1). When soybean yield was compared based on IRG usage (forage versus green manure), Ko+CC showed a 19% greater yield compared with Ko−CC, and Win+CC showed a 34% higher yield compared with Win−CC (
Table 4). Furthermore, the average grain yield of the IRG-treated sample was 2.18 Mg ha
−1 compared with 2.00 Mg ha
−1 for F. The average of +CC (2.43 Mg ha
−1) was 22 and 26% greater compared with F (2.00 Mg ha
−1), and the average of −CC (1.93 Mg ha
−1), respectively. This pattern of response was similar to 2021 LAI values at the R4 stage (See
Section 3.4).
In 2022, Ko+CC (1.87 Mg ha−1) and Win+CC (1.89 Mg ha−1) had the highest grain-yield values, while Win−CC (1.30 Mg ha−1) had the lowest value. Grain yield for Win+CC was 45% greater than the Win−CC. The average of +CC (1.88 Mg ha−1) was 20 and 32% higher compared to F (1.57 Mg ha−1) and −CC (1.42 Mg ha−1), respectively. In the comparison between years, it was observed that 2020 received more rainfall in July compared to 2021. However, there was no significant difference in soybean grain yield, while the yield in 2022 was 24% lower than in 2021 (p = 0.0013).
3.2. IRG Above- and Below-Ground Biomass
The above- and below-ground biomass of two different ecotypes of IRG were compared for 3 years (
Table 5). Only a year main effect occurred for IRG below-ground biomass (
p = 0.0274). On average, IRG above-ground biomass yield was 6.6, 6.4, and 7 Mg ha
−1 of dry matter for 2020, 2021, and 2022, respectively. This was slightly less than in a previous study (8.7 Mg ha
−1 of dry matter) in Korea with the Kowinearly cultivar [
19]. In 2022, IRG below-ground biomass was 46 and 41% lower than the average of 2020 and 2021 (average of 1.3 versus 2.4 and 2.2 Mg ha
−1 of dry matter). However, if IRG was used as a green manure (+CC), the sum of biomass incorporated into the soil was 9.0, 8.6, and 8.3 Mg ha
−1 of dry matter in 2020, 2021, and 2022, respectively. Thus, with different usage scenarios such as green manure (+CC) versus forage (−CC), dry-matter input to soil can differ by up to 7-fold.
3.3. IRG Above-Ground Biomass Nitrogen Content
To estimate the nitrogen supply to soybeans from IRG above-ground sources, IRG above-ground nitrogen content was measured (
Table 6). Significant differences were observed in the main effect of Year (
p < 0.0001). The IRG nitrogen content in 2020 (151 kg ha
−1 of N) was 80 and 62% higher than in 2021 and 2022, respectively. No significant variations in IRG nitrogen content were found across different IRG cultivars. This may indicate that IRG above-ground incorporation did not affect soil organic matter (
Table S1). Additional input of N from IRG above-ground may have contributed to the increased soybean grain yield of +CC treatments (
Table 4) as compared to F or −CC.
3.4. Soybean LAI and Chlorophyll Content
To understand the photosynthetic capacity of soybean during the growing season, LAI and chlorophyll contents were measured during 2021 and 2022 (
Table 7). For LAI, there was a treatment × growth-stage interaction in 2021 (
p = 0.0388), while there was a growth-stage main effect only in 2022 (
p < 0.0001). Hence, chlorophyll content showed growth-stage main effects for both years (
p < 0.0001), and there was a treatment main effect in 2021 (
p = 0.0061).
Specifically, Ko−CC treatment had the highest LAI value of 1.8 at V7 stage in 2021. The average LAI of IRG-treated plots was slightly higher than F at V7 (1.5 versus 1.3). There were no differences among the treatments at R2. The mean LAI values were 3.2, 3.1, and 3.6 for F with an average −CC, and +CC, respectively, at R4. In 2022, the average LAI values at R5 were the greatest and followed by R2 and R1 (5.3, 3.6, and 2.4, respectively). At R1, F tended to have the lowest LAI value (2.2), while the IRG-treated plots had an average LAI of 2.5. However, there were no statistical differences between the treatments.
In 2021, the chlorophyll content of Ko+CC was greatest (369 mg m−2), while Ko−CC had the lowest value (354 mg m−2) averaged across growth stages. The average value for each growth stage was greatest during R3, followed by R6 and R1 (398, 376, and 312 mg m−2, respectively). In 2022, the chlorophyll content was highest during R3, followed by R2 and R6 (374, 334, 288 mg m−2) across the treatments. Interestingly, the chlorophyll content at R6 in 2021 (376 mg m−2) was 31% higher than that of the R6 stage in 2022 (288 mg m−2), suggesting that the soybean stay-green period was maintained through the later reproductive stage in 2021. There was no difference in chlorophyll content between different usages of IRG in either 2021 or 2022.
3.5. Soybean Total Root Length, Surface Area, and Volume
To investigate the differences in root development in early (vigorous growth), middle (maximum development), and late (before major decline) plant developmental periods, measurements of total root length, surface area, and volume were conducted for 3 years. The total root length, surface area, and volume showed significant treatment × growth stage interactions in 2020 (p < 0.05). In 2021, treatment- and growth-stage main effects were observed (p < 0.05). In 2022, treatment- and growth-stage interactions were observed only for total root length and volume, while significant differences were observed in total root length, surface area, and volume under the main effect of growth stage (p < 0.0001).
In 2020, the total root length, surface area, and volume in the plants showed significant differences among the treatments at R3, with the highest values observed at this stage (avg. of 2030 cm, 286 cm
2, 8.3 cm
3,
Table 8). Among the treatments at R3, the average total root length, surface area, and volume in the plants were highest for the −CC avg., measuring 2580 cm, 373 cm
2, and 11.2 cm
3, respectively. When different IRG usage was compared with the F using preplanned contrast at R3, the total root length was 62% greater for avg. of −CC (2580 cm) and 35% overall IRG-treated (2148 cm) than that of the F (1590 cm) (
Table 9). Similarly, the total surface area was 70% greater for avg. of −CC (373 cm
2) and 38% overall IRG-treated (303 cm
2) than that of the F (219 cm
2) (
Table 9). Similarly, the total volume was 78% greater for avg. of −CC (11.2 cm
3) and 40% overall IRG-treated (8.8 cm
3) than that of the F (6.3 cm
3) (
Table 9).
In 2021, across the growth stages, total root length, surface area, and volume in the plants were the highest trend in Win−CC with values of 1980 cm, 382 cm
2, and 6.4 cm
3, respectively. Among the growth stages, R3 showed the largest average values for total root length (2620 cm) and surface area (429 cm
2), followed by R6 and V7 (
Table 8). When comparing F using preplanned contrasts at the R3 stage, total root length significantly increased by 8% (
p = 0.0319) under an average of +CC (2475 cm) compared to F (2290 cm). At the R6 stage, total root volume showed a significant 33% increase (
p = 0.0215) with an average of −CC treatment (8.8 cm
3) compared to F (6.6 cm
3).
In 2022, the total root length showed significant differences between the treatments at R3. The Win+CC had the greatest length (3720 cm), while Ko+CC had the smallest (2220 cm). The total root length of Ko−CC was 40% greater for Ko+CC (3100 versus 2220 cm), and Win+CC was 39% greater for the Win−CC (3720 versus 2670 cm). When comparing between growth stages within a treatment, Ko−CC and Win+CC had a greater total root length at R3. When different IRG usages were compared with F using preplanned contrast at the R3 stage, the IRG-treated (2928 cm) and the average of −CC (2885 cm) and +CC (2970 cm) resulted in total root length increases of 15% (
p = 0.0008), 13% (
p = 0.0152), and 16% (
p = 0.0002) compared to that of the F (2550 cm). In the case of total root surface area, the average values across treatments were relatively higher at the R3 and R6 (
Table 8). The total root volume at the R3 stage was greatest for Ko−CC, while Ko+CC had the smallest (7.5 versus 4.4 cm
3). At the R6 stage, Win−CC had the highest volume, while Ko+CC had the lowest (11.9 versus 6.5 cm
3). Unlike total root length, root volume had the largest value at R6 across the treatment. When different IRG usage was compared with F using preplanned contrast at the R6 stage, the average of the −CC group was of 12% greater root volume compared to F (10.9 versus 9.7 cm
3) (
p = 0.0028). Overall, the total root length, surface area, and volume in the plants for both R3 and R6 tended to have greater values in 2022 compared to 2021 (
Table 8).
4. Discussion
To understand the effects on above- and below-ground soybean development, various IRG-soybean rotation regimes were compared for 3 years under field conditions. Soybean yield component analysis indicated IRG usage as a green manure (+CC) had generally greater grain yield than other treatments, while IRG for forage (−CC) was not different from F across IRG cultivars. This is in line with previous studies that found higher soybean grain yields when both the above-ground and below-ground parts were placed as cover crops in comparison to F [
20]. In addition, the introduction of a cover crop increased soybean yield by 14% compared with no cover crop [
9]. In contrast, it differed from previous research where the soybean grain yield following IRG cultivation was lower than that after winter fallow [
21]. A previous cover crop treatment showed that there was no significant difference in soybean yield compared to no cover crop control [
8]. It is likely that the increased input of organic matter and subsequent mineralization in +CC compared with −CC positively influenced soybean grain yield (
Table 4). There was also a difference among years in soybean grain yield. The overall mean of the treatments in 2022 was significantly lower than in 2020 or 2021 (
p = 0.0013). This significant decrease in grain yield can be attributed to the reduced rainfall in 2022, particularly during the reproductive stage (
Table 2). This is in line with previous studies where yield reduction occurred due to water stress during the reproductive growth stage of soybean [
22,
23]. Particularly, the precipitation in August was reduced by 200 mm and 163 mm in comparison to 2020 and 2021, respectively (
Table 2). This period corresponds to the developmental stages of pod development (R3–R4), during which drought stress has an impact on grain yield [
24]. In addition, GDD in 2022 was lower by 6 and 77 °C compared to 2020 and 2021 in October, respectively (
Table 2). Lee et al. (2022) suggested that conditions with higher GDD levels are favorable to an increase in soybean grain yield [
25]. Therefore, it appears that the combination of drought conditions and lower GDD resulted in reduced grain yield. Thus, for 3 years of study indicated that even under unfavorable weather condition, +CC treatments showed greater yield compared to other treatments.
The above- and below-ground biomass of two different ecotypes of IRG showed that IRG below-ground biomass in 2022 was 43% lower than the average of 2020 and 2021. This was also due to a different weather pattern for each growing season (
Table 2). Even though the above-ground biomass yield was not affected by the year, lower precipitation during the winter-growing season negatively affected root development. Specifically, the third-year winter growing season had lower precipitation than the previous two years (435, 434 versus 233 mm; November to May). Previous studies addressed that under moderate drought-stress conditions, wheat exhibited reduced root mass in both topsoil and subsoil compared to well-watered conditions [
26]. Previous research indicated that as soil penetration resistance increased, root length density decreased in the compacted soil layer [
27,
28]. Under moderate water stress, the decrease in root weight was more pronounced than that of above-ground biomass [
29]. Despite large differences in dry matter input among IRG-treated plots (
Table 5), there was no difference in soil organic matter content among the treatments (
Table S1). According to previous studies, only 10–20% of dry matter input becomes part of the soil organic matter [
30]. Although the amount of biomass input to soil was significantly different, actual differences in the organic matter pool may have been unaffected among treatments.
Starter fertilizer to soybean is a common practice as prior research indicated that supplying 50 kg ha
−1 of starter nitrogen fertilizer resulted in the highest soybean grain yield [
31]. Based on the IRG above-ground biomass nitrogen content analysis, the amount of N supply from +CC exceeded suggested initial N fertilization of the previous study. Thus, to promote the initial growth of soybeans, implementing crop rotation with IRG as a cover crop may be an alternative method of using inorganic nitrogen starter fertilizer. This is in line with the recommendation of the previous study that use of a gramineous cover crop stored 25% more N on the soil surface than no cover crop control and may replace starter N fertilizer [
32]. Above-ground IRG had 79–156 kg ha
−1 of N, which subsequently decomposed; incorporated IRG could be served as a starter fertilizer. Previous studies also reported that N accumulation of 26 kg ha
−1 from buried oat straw and 39 kg ha
−1 from cereal rye residue could be supplied to following crops [
33,
34]. Sievers and Cook (2018) observed that cereal rye residue exhibited a slower and more gradual release of nitrogen compared to hairy vetch, emphasizing the need for optimal synchronization of cover crop nitrogen release with subsequent crop nitrogen uptake to reduce nitrogen fertilizer [
35].
The soybean LAI of IRG incorporated (+CC) had relatively higher values than other treatments for 2021 at R4. This is similar to a previous study that LAI of soybean at the R4 stage was 41% higher when the cover crop was incorporated compared with the no-cover crop control [
20]. It is reported that under abiotic stress conditions, rice exhibited higher LAI and yield when intercropped with green manure, compared to the control conditions [
36]. Previous studies also indicated that when the LAI of soybean during the R1–R4 stage ranges from 3.5 to 4, the photosynthetic potential is maximized [
37,
38]. The chlorophyll content is a crucial indicator reflecting the photosynthetic activity of plants [
39]. In this study, the chlorophyll content during the R3 and R6 stages decreased sooner in 2022 compared to that of 2021, likely due to reduced rainfall in July and August (
p < 0.0001,
Table 2). Elsalahy and Reckling (2022) reported a 7% reduction in chlorophyll content of drought-stressed soybeans during the vegetative and flowering stages compared with under rainfed conditions [
40]. Gholamin et al. (2011) also observed that drought stress diminished chlorophyll content and yield while also revealing a strong correlation between chlorophyll content and harvest yield [
41]. Therefore, the decrease in chlorophyll content during the R3 and R6 stages occurred due to drought conditions in 2022 regardless of IRG input regimes.
In 2020, the total soybean root length, surface area, and volume was greater for IRG-treated crops than that of the F across the IRG cultivars. It was reported that as the root length density of the cover crops (triticale and pearl millet) increases, there is a corresponding increase in soybean root length density in 5–10 cm of soil [
42]. Additionally, it was noted that the vigorous root growth of triticale and pearl millet led to a reduction in soil-penetration resistance [
42]. During favorable conditions in 2020 and 2021, −CC showed a tendency for greater soybean total root length and surface area than +CC. When plants had moderate nutrient depletion, they tend to develop excessive roots to scavenge the nutrients and water. It was reported that low phosphorus concentrations lead to a high density of long roots [
43]. Lecompte et al. (2008) observed a 180% increase in root length when nitrogen was limited compared to when it was sufficient [
44]. Additionally, they observed an enhanced root density extending into deeper soil layers under conditions of low-soil nitrogen levels, and they characterized root expansion as continuous across the entire soil profile [
44]. In the current study, this is probably why there were root development differences in later growing seasons between −CC and +CC. Hence, due to the predominant contribution of fine roots at root length, the total root length was significantly influenced by fine root development [
45]. Fine roots are directly associated with water uptake compared to main roots, and they enable stable crop production through root distribution and development [
46]. In the current study, overall root length development was highest at R3 in 2022, and Win+CC had the highest total root length. This indicates fine root development reached maximum at R3, suggesting Win+CC probably had greater adaptability to unfavorable weather conditions, including drought. The previous research suggested that the substantial proportion of fine roots in the root domain allows for the optimization of the capacity to explore the soil in preparation for drought conditions [
47]. Thus, the current study suggested that incorporating IRG in soybean production may enhance the root system of soybeans and soybean yield.
In later seasons (R3 and 6), the total root length, surface area, and volume tended to have greater values in 2022 compared to 2021 (
Table 8). This can be attributed to an overall lower precipitation, particularly during the months of July and October in 2022, leading to the development of larger and elongated roots for enhanced water acquisition (
Table 2). Fenta et al. (2014) reported that most cultivars had increased root length, surface area, and volume under drought conditions, excluding drought-sensitive varieties [
48]. Hence, it was reported that ruzigrass was found to enhance the growth of soybean roots in compacted soil conditions compared with other preceding crops (maize, oat, and wheat) [
49]. Additionally, it has been suggested that the continuous presence of biopores created by ruzigrass in the preceding crop can promote soybean root growth even under water-stressed conditions, potentially leading to increased yields [
49]. According to the previous study, cover crops resulted in an approximately 80% increase in water infiltration compared with no cover crop [
9]. Basche et al. (2016) reported that a previous cover crop treatment increased soil water content at a depth of 30 cm relative to the no-cover crop [
8]. Therefore, it can be suggested that the increased water-holding capacity due to the cover crop may have contributed to enhanced soybean root growth and maintenance.
When overall yield was compared between years, the yield in 2022 was lower compared to the years 2020 and 2021 (
Table 4). This is attributed to the extended development of root volume and LAI during later seasons (
Table 7 and
Table 8). This is most likely due to the drought in 2022, which disrupted nutrient flow as plants progressed from the vegetative stage to the reproductive stage. Islam et al. (2019) suggested that the decline in LAI during the reproductive stage could be attributed to a reduction in leaf nitrogen concentration required for grain filling in rice [
50].