4.1. Interaction Water and B Deficits on Biomass Accumulation, B and N Uptake under Controlled Conditions
On the treatments with adequate nutrition with B and without water stress, a decreasing acropetal gradient was observed in the B content between mature and youngest leaves from 267,07 to 63,72 mg.kg
-1 (
Table 4). The decreasing acropetal gradient in the treatments without water stress without B, and with water stress without B reversed, changing to an increasing acropetal gradient, from 9.56 to 12.72 mg.kg
-1 in the treatment without water stress without B and from 80.54 to 249.14 mg.kg
-1 in the treatment with water stress and without B (
Table 4). These results suggest that the B translocation from mature to young leaves can occur at a low B supply, in plants grown with and without water deficit. This process was well described by Brown and Shelp [
15] for several crops like broccoli, soybean, cotton, grapes, and peanuts. In those crops, a decreasing acropetal gradient of the B concentration was found when grown with luxury or adequate B supply. However, the authors report that when those crops were grown with a B deficit, the gradient from old to young tissues disappeared or reversed.
Changes on the B concentration between mature to young leaves under water stress conditions, suggest a B remobilization of B under water stress conditions, that was not observed on the well-watered treatments (
Table 4). Considerable evidence suggests that B can be transported to sink tissues of many species in the phloem [
15,
40,
41,
42]. This B mobility in the phloem can occur in any species in which sorbitol is a primary photosynthesis product. Polyols like sorbitol, mannitol, and or dulcitol can effectively complex B [
42,
43] (Brown and Hu, 1998; Du et al. 2020). Mannitol is one of the most widely distributed polyols and is present in over 100 higher plants including the Rubiaceae to which Coffee belongs [
44].
Leite et al. [
41], utilizing isotopic B labeling provide evidence that B remobilization occurs in coffee trees, with small translocation in well-nourished plants (without B deficit), but significant phloem translocation or remobilization at deficit supply of B, like what is reported in this research for the treatments without drought stress without B. Olivera-Silva et al. [
45], demonstrated a B remobilization in Cowpea (
Vigna unguiculata (L). Walp), which in turn resulted in a high B accumulation and a significant increase in the dry biomass accumulation. Bellato et al. [
46] report more than 50% of the B contained in coffee leaves was found in the cell wall fraction with the remaining B being soluble. This shows implies that the B fraction in coffee cells that is not complexed is relatively high and hence may be available for remobilization. In citrus plants, Boaretto et al. [
47,
48] reported B remobilization from older tissues, estimated that 30-35% of total boro in the leaves of new flush were remobilized from plant reserves.
In both water levels (with and without drought stress), the N content in young and mature leaves was significantly higher in the treatments without B (
Table 4). This could be explained by the influence of B on the N metabolism. The influences of B on the N assimilation can be observed in the coffee plants that were grown with water deficit: Treatments with water stress with and without B supply did not show significant differences in the N uptake, but the N content in young and mature leaves in the treatments with B supply was significantly lower (
Table 4) and the biomass accumulation significantly higher (
Figure 1). Wang et al. [
49] report significant improvement in the N uptake, NUE, and yield in Rapeseed (
Brassica napus) with the application of B fertilizer, with a higher benefit of the B application on higher N rates (180 kg N.ha
-1) than in the treatments without and/or lower N rate.
The way how these micronutrients affect the drought sensitivity in plants could be explained in two ways. Firstly, B together with Zn and Mn are involved in the detoxification of ROS playing a protective role in preventing photooxidative damage catalyzed by ROS in chloroplasts. Secondly, these micronutrients might greatly contribute to drought-stress tolerance by protecting against oxidative damage to membranes [
50,
51]. The levels of ascorbic acid, non-protein SH-compounds (mainly glutathione). and glutathione reductase, the major defense systems of cells against toxic O
2 species, are reduced in response to B deficiency [
51]. Yan et al. [
52] working in citrus, growing with and without acid stress “excessive H
+ protons at pH of 4,0”, demonstrated that the application of B protected plant roots from H
+-toxicity by inhibiting the outbreak of ROS in the roots and regulating the protective monachism of antioxidant enzymes.
B is essential for organisms with carbohydrates-rich cell walls, and symptoms of B deficiency include the cessation of growth of apical meristems (both shoot and roots) and the development of brittleness of leaves which has been ascribed to an inhibition of cell wall synthesis or structural integrity. B deficiency also results in the formation of abnormally thick and structurally deformed cell walls [
24]. The most frequent B deficit symptoms observed in this research were: a deformation and the presence of brown spots on the youngest leaves. When the leaves reach a month of development a discoloration appears on the outer edge of the leaves. The most severe symptom of the B deficit was a descending branch death or cessation of growth of the apical shoot meristems and necrosis of the tissues (
Figure 2B). This descending branch death has been associated with environmental stresses such as soil and atmospheric water deficits, high temperature, high insolation, N deficits, or a combination of all [
53]. In the juvenile phase of coffee growing, the death of branches does not represent a problem, it is however frequently seen in productive plants [
53]. We observed this physiological disorder also in juvenile plants growing without B. Branch death was also often observed in the field trial after 3 years of the treatment without Ca
+2 and B, which also explains the significant differences in productivity at the end of the productive cycle (
Figure 1).
The optimum foliar B concentration for coffee in the third and fourth pair of leaves is considered normal between 60 to 80 mg.kg
-1 [
21,
54]. In this research, in well-watered conditions, the highest biomass accumulation was achieved with a B content in the young leaves of 63,72 mg.kg
-1 and in mature leaves of 265,07 mg.kg
-1. However, under water stress conditions, due to the remobilization of B, the highest biomass accumulation was achieved with a B content in young leaves of 249,14 mg.kg
-1 (without toxicity symptoms) and 80,54 mg.kg
-1 in mature leaves (
Table 7).
4.2. Sinergy Ca-B on Coffee Productivity
The yield in 2017 was high in all treatments (
Figure 3), because the coffee plantation was young (3 years after pruning) and because of the high net precipitation and ETc during the period 2016-2017. The net rainfall in 2016-17 was almost 2 times higher, and the ETc was 73% higher compared to the previous period 2015-2016 (
Table 5). The period 2015 to 2016 was influenced by the Pacific South Oscillation ENSO (El Niño-La Niña) conditions, which were in a positive phase known as El Niño [
55,
56]. El Niño for the study area resulted in an increase in the mean-air temperature, an increase in solar radiation (
Table 1), and a reduction in the rainfall. For the coffee plantation, this reduction in the rainfall during the tree growth and coffee cherries development results in a decline in growth, yield, and quality of the coffee [
5,
8]. A stress period after harvest and during pre-flowering, however, has a positive influence on productivity through better flower induction [
57,
58].
Application of an average rate of 77 kg CaO and 1,1 kg.B.ha
-1.year
-1 improves the coffee yield in the 4
th year of application (
Figure 3), and the B content in the soil (
Figure 4), compared to the treatment with the same Ca
+2 rate with less B (0.6 kg.B.ha
-1.year
-1), and control without both nutrients indicating the importance soluble Ca
+2 and B in coffee in long term. Boron nutrition in crops is a challenging practice, due to the high mobility of B in many soils, its high adsorption capacity and the narrow window between deficiency and toxicity [
59,
60,
61]. In Arabica coffee in Brazil, Santinato et al. [
54] found an application of B at a rate higher than 2,0 kg. B. ha
-1 linearly reduces the yield by 0,33 coffee bags. ha
-1 (0,02 t of green coffee bean.ha
-1) per kg of B applied in excess of 2,0 kg. B. ha
-1. In contrast Cong, [
62], working on a 10-year-old Robusta coffee plantation during one season in highly acidic soil in Vietnam (Basaltic soil of Central Highlands), reported an average yield increase of 10,2% with the application of 3,0 kg B. ha
-1. These results indicate that the response to nutrition in B is variable according to the coffee species, and environment.
The additive effect between B and Ca
+2 after long-term application observed in the field trial can also be explained by the influence of both nutrients on the cell structure of coffee plants, both nutrients has been reported as a key nutrient in coffee plants, influencing metabolic structural and morphological processes [
28,
31]. B act in the biosynthesis of the cell wall, assisting Ca
+2 in the deposition of pectates in the cell wall. Boron also forms cis-diol-borate complexes, which are constitutional elements of the plasmalemma [
63].
A similar interaction between B and Ca
+2 was also described by Brown et al. [
24], where the Ca
+2 and B play a cooperative role in the stabilization of the membrane by the formation of a mixed complex in which Ca
+2 binds to polyhydroxyl borate esters or by direct association with different compounds of the membrane. In
Vicia faba roots, the membrane-bound Ca
+2 decreased within several hours of B deficient conditions due to the reduction of specific Ca
+2 -binding sites (borate esters with vic-diols or polyhydroxil- carboxylates) before plasma membrane integrity deteriorates [
64]. Synergies between Ca and B and their influences on crop productivity also have been reported in a 3 years trial in Cranberries by DeMoranville and Deubert, [
65]. The authors found a yield increase of 24 to 31% with foliar Ca and B applications during the period of strong vegetative growth and floral development, and recently by Galeriani et al. [
66] who report significant improvement in gas exchange parameters, water use efficiency and yield in soybean.
4.3. B in the Soil After Five Years Application
For coffee, in contrast to other crops such as barley or cauliflower [
67,
68], a science-based definition of critical levels of B in the soil following the soil test calibration approach described by Kidder, [
69] is lacking. The local institutes or universities have defined empirically the critical levels, based on local expert knowledge. Malavolta et al. [
29], for example, proposed a low level below 0,4 mg.kg
-1, a medium level between 0,4 to 0,8, and higher levels when B is higher than 0,8 mg.kg
-1. In our trial the higher yields were achieved with a B level in the soil of 1,17 mg.kg
-1 in the soil using the CAT extraction methods (within a confidence interval of 0,86 to 1,49 mg.kg
-1).The treatment without B and Ca showed significantly lower coffee yield after four years of harvest and low B content in the soil of 0,28 mg.kg
-1, much lower than the B content at the start of the trial (0,38 mg.kg
-1).
4.4. B and the Biochemical Composition of the Green Coffee Beans in Field Conditions
The chemical characteristics of green coffee beans are determined by the combination of three main factors:
Environmental x Genetic x Agricultural practices [
70]. The chemical components of roasted coffee can be grouped into volatile and non-volatile substances. Non-volatile compounds such as caffeine and lipids together with sugars, trigonelline, and chlorogenic acids influence the beverage quality [
71,
72]. Caffeine has negative and significant correlations with all cup quality attributes of coffee such as acidity, body, flavors, and overall standard of the liquor [
73], and is mostly associated with the bitterness in the coffee cup [
71,
74]. Fatty acids, as constituents of the lipid fraction, contribute to the aroma, flavor, and mouth feel perceived which are usually influenced by the type and concentration of lipids [
71]. Saturated fatty acids including arachidic (C20:0), stearic (C18:0), and palmitic acid (C16:0) have been described as a potential discriminator of specialty coffees, indicating better sensory quality. In contrast, unsaturated fatty acids (UFAs), such as oleic (C18:1), linoleic (C18:2), and linolenic (C18:3) acids have been related to a coffee beverage with less intense acidity, fragrance, and flavor [
75], and have also been linked to a loss of sensory quality during storage [
76].
The significant differences in caffeine, and some fatty acids specially C18:1; C18:2, and C18:3 between 2016 and 2019, is explicable by the changes in the rainfall and ETc generated by the ENSO conditions. During the period 2015-2016 correspondent with the harvest of 2016, the climate conditions were warmer, and dryer compared with the period 2018-2019, with 58% less net rainfall and 47% lower ETc (
Table 5). The water stress and foliar B application can alter the seed composition in soybeans [
77], with an increase in the oleic acid concentration under water stress compared to non-stress conditions, without changes in linolenic acid concentration. In both conditions, with and without stress, foliar B application resulted in an increase in oleic acid and in a decrease in linolenic content.
Fatty acids and mainly UFAs are recognized as important in the general defense systems against various biotic and abiotic stresses [
78]. In plants, fatty acids (FA) are crucial components of cellular membranes, suberin, and cutin waxes that provide structural barriers to the environment and contribute to inducible stress resistance through the remodeling of membrane fluidity, and as modulators of plant defense gene expression [
79]. DaMatta and Ramalho, [
4], associated the better acclimation of some coffee genotypes to abiotic stress conditions (cold stress) with the increase in the saturation of FA in the membrane that reinforced the antioxidative system. Wu et al. [
80] demonstrate that B deficiency causes structural and morphological changes in trifoliate oranges roots. B deprivation-induced ROS accumulation accelerated the membrane peroxidation, resulting in weakened cell vitality and cell rupture in roots. Chen et al. [
81] found that B deficiency led to an excessive accumulation of phenolic compounds in alfalfa seeds. In this paper, we report a negative correlation between caffeine and B content in green coffee beans (
Table 7)
B deficiency caused an increase in the cytosolic calcium concentration (Ca
+2 cyt) in
Arabidopsis thaliana roots after 6 and 24 h of this nutrient deficiency. The (Ca
+2 cyt) was gradually restored with B application or when B-sufficiency conditions were established [
82].