Soybean Micronutrient Content in Irrigated Plants Grown in the Midsouth

Concentrations and contents of iron (Fe), boron (B), zinc (Zn), manganese (Mn), and copper (Cu) were determined for two MG IV and one MG V irrigated soybean (Glycine max L. Merr.) cultivars grown on clay and sandy loam soils in 2011 and 2012. Plants were sampled at V3, R2, R4, R6, and R8, tissues separated, dried, weighed, and nutrient concentrations determined. Nutrient contents were calculated. No cultivar, site, or year differences in nutrient concentrations or contents were observed. Iron had the greatest concentration and content of all followed by B, Zn, Mn, and Cu. Maximum concentrations and contents in leaves occurred at R4 and later declined. Concentrations and contents in stems remained constant or increased while pods rapidly increased until (R8). A 3328 kg ha^?1 seed yield will remove 325.0 g Fe ha^?1, 153.9 g B ha^?1, 175.6 g Zn ha^?1, 100.0 g Mn ha^?1, and 52.5 g Cu ha^?1.     

Agronomic bio-fortification and quality enhancement in okra–pea cropping system through arbuscular mycorrhizal fungi at varying phosphorus and irrigation regimes in Himalayan acid alfisol

A field experimentation was conducted during 2009-2011 at CSK Himachal Pradesh Agricultural University, Palampur, India characterized with wet-temperate climate and acid Alfisol soil having medium available phosphorus content. The study aimed at bio-fortification and quality enhancement of okra (Abelmoschus esculentus)–pea (Pisum sativum) cropping system through arbuscular mycorrhizal fungi (AMF) (Glomus mosseae) at varying inorganic phosphorus (50, 75, and 100% soil-test-based recommended P dose) and irrigation regimes (40 and 80% available water capacity) in a Himalayan acid Alfisol. The results revealed that AMF and inorganic P significantly enhanced the concentrations and uptake of various primary [nitrogen (N), phosphorus (P), and potassium (K)]; secondary [calcium (Ca)]; and micronutrients [iron (Fe), zinc (Zn), copper (Cu), manganese (Mn), boron (B), and molybdenum (Mo)] in okra and pea crops. However, effects of varying irrigation regimes were found to be nominal. In okra, AMF inoculation considerably enhanced N, P, K, B, and Mo uptake by 5, 19, 3, 4, and 15%, respectively, over their non-AMF counterparts. Likewise in pea, a higher amount of N (10%), P (26%), K (7%), Fe (7%), Cu (38%), Zn (20%), Mn (4%), B (7%), and Mo (13%) uptake was registered through AMF inoculation over their non-AMF counterparts. Application of soil-test-based P dose from 50% to 100% P also resulted in significant and consistent improvement in N, P, K, B, and Mo uptake both in okra and pea and in Zn, Cu, Mn, and Fe uptake in pea crop. Magnitude of increase in Ca content was to the tune of 13 and 4%, respectively, in okra fruits and pea pods following AMF inoculation, whereas crude protein content enhanced by 4% each in both the crops. Overall, the current study demonstrates the important role of AMF in nutrient enrichment and quality enhancement of okra and pea crops in acid Alfisol, besides considerable reduction in investment on chemical fertilizers. Results of current study suggest that AMF use in Himalayan production systems is of tremendous significance to harvest nutritionally-rich farm produce for Himalayan communities suffering from malnutrition especially anemia and Zn deficiency, and equally to resource-poor Himalayan farmers who ill-afford expensive external inputs.     

Spatial variability and evaluation of status of micronutrients in selected soils around Taihu Lake, China

Background, aim, and scope  Soil micronutrients are essential for plant growth and human health. Spatial variability and evaluation of soil micronutrient status are the research hotspot. The plain of northern Zhejiang Province, around Taihu Lake, China, is a key agriculture production area. With the rapid development of agriculture in Zhejiang Province, the management of soil micronutrients is of increasing concern to sustain crop productivity and human health. Soil-available micronutrients in the study region have not previously been studied in detail. Primary objective of this research was to examine the spatial distribution and evaluation of soil-available micronutrients in the arable land in this agriculturally important region using geostatistics. The controlling factors for the spatial variability of available micronutrients were interpreted. The research findings attained in the present study are of fundamental significance in providing a guideline for precise agriculture management practice and sustaining food security. Materials and methods  Amounts of available Fe, Mn, Cu, Zn, B and Mo in 1893 soil samples taken from the arable land in nine counties in northern Zhejiang Province, around Taihu Lake, were measured and their spatial distribution patterns were investigated. Available Mn, Fe, Cu, and Zn were extracted with DTPA and analyzed by inductively coupled plasma–atomic emission spectroscopy. Available B was extracted with boiled water, then determined by inductively coupled plasma–optical emission spectroscopy. Available Mo was extracted with Tamm reagent and was then determined by inductively coupled plasma-mass spectrometry. Geostatistics was conducted for the data processing. Results  More than 50% of the arable land were deficient in available Mo, while more than 70% had extremely low amount of available B. Amounts of available Cu, Zn and Mn were relatively high, whereas the soils are extremely sufficient in available Fe. The geostatisticical data shows that Mn, Cu, Zn, and Mo were best fit with an exponential model, while Fe and B were best fit with a spherical and linear model, respectively. Copper and Mo had strong spatial dependency, which is attributable to the effects of natural factors including parent material, topography, and soil type; Fe, Mn, and Zn had medium spatial dependency; however, B had weak spatial dependency, indicating an involvement of anthropogenic factors. Nevertheless, the six micronutrients studied all show spatial distribution trend to a certain extent. Discussion  Based on the provincial classification standard of soil micronutrients and the results of the present study, regionalized management of soil micronutrients was recommended. We divided the soil micronutrients investigated in the present study into three types: Type I (Fe), Type II (Mn, Cu, and Zn) and Type III (B and Mo). Type I is sufficient, and its amount needs to be controlled; otherwise, it will be toxic to crops. Type II is enough and its amount does not need to be increased currently through micronutrient fertilization. However, Type III is deficient in substantial areas in the region studied and its cause of deficiency needs to be investigated; its availability needs to be improved to sustain the crop production and food quality. The availability of B and Mo in the north of Zhejiang Province should be regionally managed. Over the past two decades, the spatial variability of soil-available micronutrients in the study region was attributable to the soil formation factors as well as anthropogenic activities such as fertilization, cultivation, and other soil management practices. The lower available B and Mo concentrations in the arable land were apparently due to continuous cropping and intensive applications of fertilizers without adequate supply of micronutrients. The high available Fe and Mn concentrations in the soils were attributed to increasing soil acidification and relatively high soil organic matter contents. The high available Cu and Zn levels of the soils in this region were attributed to intensive utilization of animal manure as fertilizers. Conclusions  Based on the provincial classification standard and the results from the present study, regionalized management of soil micronutrients was recommended. Moreover, the present study would provide an insight into understanding the basis for the development of innovative strategies for land management practices such as precision farming and environmental risk assessment. Recommendations and perspectives  The research findings attained in the present study would help to improve our understanding of spatially variable availability of soil micronutrients and providing a quantitative basis for decision and policy making to develop innovative agricultural management strategies to sustain micronutrient nutrition. Further research should be conducted to elucidate the relationship between soil micronutrient and plant growth and human health.     

Improvement of mineral nutrient content of tomato through selection of cultivars and soil fertility

Depleted soil fertility and high-yielding cultivars have been associated with low nutrient contents in vegetables. This study explored if elemental nutrient concentrations in tomato (Lycopersicon esculentum Mill.) can be increased through selection of cultivars and nutritional regimes. Cultivars with different phenotypes of heirloom and modern origins were studied in field experiments in two years. Chemical fertilizer (10-10-10), compost, and an organic fertility regime of soybean meal, bone meal, and potassium sulfate were assessed for their effects on growth and composition of fruits of the cultivars. Differences in nutrient concentrations between modern or heirloom cultivars or among fertility treatments were small or non-significant. Differences among individual cultivars for each element were large with some cultivars having nearly twice the concentrations of nutrients of others and with considerable uniformity in cultivar rankings among the elements. This work suggests that cultivars can be selected for production of nutrient-dense tomatoes.     

Dry matter production,nutrient accumulation,and nutrient partitioning of barley

Total dry matter (TDM) and nutrient accumulation, nutrient partitioning, and cumulative growing degree days at the time of maximum nutrient accumulation for two‐row spring barley (Hordeum vulgare L.) are not well quantified under high‐yielding irrigated conditions common in the semi‐arid western United States. Thus, five cultivars of barley were grown under irrigated conditions on a loam soil in the 2015 and 2016 growth seasons to determine these factors. Total nutrient accumulation was greatest at either the soft dough or maturity stage where specific nutrients were greater at one stage as compared to the other. Mean N accumulation was greatest at the soft dough stage (256 kg ha^?1) where the regression model accounted for 80% of the variation in the data. Additionally, spike N increased from 91 to 105 kg ha^?1 from soft dough to maturity. Specific nutrients (e.g., K) had significantly greater plant (i.e., culms plus leaves) accumulation between soft dough and maturity, 253 and 172 kg ha^?1, respectively, where the spike at the same growth stages had an accumulation of 37 and 42 kg ha^?1, respectively. In contrast, other nutrients (e.g., P) were remobilized to the spike as noted by the increase from 14 kg ha^?1 at soft dough to 26 kg ha^?1 at maturity. In addition to nutrient partitioning, linear regressions resulted in well‐correlated models between TDM and total nutrient accumulation (R² = 0.35–0.88) for measured nutrients. Results from the current study provide critical data on nutrient accumulation as well as regression models for two‐row barley under high‐yielding conditions. This information can be used to improve harvest decisions as well as more accurately predict nutrient cycling in barley cropping systems.     

Mycorrhizal,nutritional and virgin olive oil parameters affected by groundcovers

Management of olive groves faces the challenge of reconciling yield, soil degradation and virgin olive oil (VOO) quality. We evaluated the effect of replacing tillage management by vegetal groundcovers (GC) on the relationships between mycorrhizal symbiosis, olive nutritional status, and VOO quality under field rainfed conditions. The experiment was set up in 2014 in an existing Cornicabra olive orchard with a Haplic Gypsisol soil under a Mediterranean semiarid climate. Four treatments were replicated four times and consisted of: (1) annual cover of bitter vetch, (2) permanent Brachypodium distachyon, (3) spontaneous vegetation cover (mainly Brassicaceae species), and (4) tilled soil. The use of bitter vetch GC increased the olive root colonization by 50% compared with the tillage treatment. The effect of tillage on VOO differed from that of GC use. Tillage treatment decreased maturity index and its VOO had lower polyphenol content and less luminosity than that from the GC treatments. Olive root colonization, together with changes in nutrients such as Cu, B and other elements resulting from GC use, seems to play an important role in explaining the variability of VOO quality parameters. Although tillage may lead to higher yield by controlling competition for water and nutrients, the introduction of GC in olive groves led to higher polyphenol contents, enhancing VOO quality and, at the same time, protecting soil from erosion.     

Long-term effects of intensive rice–wheat and agroforestry based cropping systems on build-up of nutrients and budgets in alluvial soils of Punjab,India

ABSTRACT

A detailed study was conducted to investigate the long-term effects of rice–wheat and poplar-based agro-forestry systems existing on a large area for last 25 years on the distribution of macro as well as micronutrients in surface soils, as well as their profiles. To achieve these objectives, profile soil samples (0–150 cm) were collected from 10 randomly scattered locations each from rice–wheat and poplar-based agro-forestry systems and analyzed for various physico-chemical properties. The results of our investigation revealed that pH, EC, OC available N, P and K reported significantly higher levels in agro-forestry as compared to rice–wheat system. On the other hand, DTPA-extractable and total Zn, Cu, Fe and Mn were significantly higher in D1 (0–15 cm), D2 (15–30 cm) and D3 (30–45 cm) depths of rice–wheat system which may be attributed to the reduced conditions prevailing during rice crop. Nutrient budgeting also assessed the impact of crop removal and fertilizer inputs along with recycling of crop residue and leaf litter. Also, the build-up of available nutrient status in surface layer (0–15 cm) and soil profiles (0–150 cm) continuously under these two systems helped in maintaining agricultural sustainability and soil fertility over a long period of time.     

SULFUR AND BORON-MAGNESIUM-ZINC COMPOUND FERTILIZER CONTRIBUTE TO THE REPRODUCTIVE GROWTH OF JATROPHA CURCAS L.

Jatropha curcas L., a native tree to Mexico and Central America, is cultivated in many counties of China as a source for biodiesel. The effects of different fertilizers on the growth of Jatropha curcas L. were studied under soil conditions of low nitrogen (N), phosphorus (P), potassium (K) and boron (B) in soil. Compared with 16N-16P-16K compound fertilizer, both sulfur (S) and a B-management (Mg)-zinc (Zn) compound fertilizer both increased the oil concentration of the seed, and promoted the reproductive growth. Only the fertilizer S increased the seed yield and the Acid value of the oil, while the B-Mg-Zn compound fertilizer declined the Acid value of the oil and induced the differentiation of female flowers. Boron-Mg-Zn compound fertilizer induced a smaller increase in the oil concentration of Jatropha curcas seed than fertilizer S and the largest increase in growth rate of trees. Moreover, Jatropha curcas showed a higher requirement of S for the reproductive phase than for its vegetative growth. Jatropha curcas may belong to the species with restricted B mobility, and B fertilizer should be sprayed as a foliar fertilizer. However, further research on the S nutrition of Jatropha curcas is required.     

Macronutrient-Use Efficiency and Changes in Chemical Properties of an Oxisol as Influenced by Phosphorus Fertilization and Tropical Cover Crops

Cover crops are important components of copping systems due to their beneficial effects on soil physical, chemical, and biological properties. A greenhouse experiment was conducted to evaluate influence of phosphorus (P) fertilization on nutrient-use efficiency of 14 tropical cover crops. The P levels tested were 0 (low), 100 (medium), and 200 (high) mg kg^?1 of soil. The cover crops tested were Crotalaria breviflora, Crotalaria breviflora, Crotalaria spectabilis Roth, Crotalaria ochroleuca G. Don, Crotalaria juncea L., Crotalaria mucronata, Calapogonium mucunoides, Pueraria phaseoloides Roxb., Pueraria phaseoloides Roxb., Cajanus cajan L. Millspaugh, Dolichos lablab L., Mucuna deeringiana (Bort) Merr., Mucuna cinereum L., and Canavalia ensiformis L. DC. Agronomic efficiency (shoot dry weight per unit P applied), physiological efficiency (shoot dry weight per unit of nutrient uptake), and apparent recovery efficiency (nutrient uptake in the shoot per unit nutrient applied) were significantly varied among cover crops. Agronomic efficiency decreased with increasing P levels. Overall, physiological efficiency of nutrient uptake was in the order of P > sulfur (S) > magnesium (Mg) > calcium (Ca) > potassium (K) > nitrogen (N). Similarly, apparent recovery efficiency was in the order of N > K > Ca > Mg > P > S. Different recovery efficiency in cover crops can be useful in selecting cover crops with high recovery efficiency, which may be beneficial to succeeding crops in the cropping systems. The P × cover crops interactions were significant for soil extractable Ca²⁺, P, cation exchange capacity (CEC), Ca saturation, Ca/K ratio, and K/Mg ratio, indicating that cover crops change these soil property differently under different P levels. Thus, cover crops selection for different P levels is an important strategy for using cover crops in cropping systems in Brazilian Oxisols. Optimal values of soil pH, soil Ca and Mg contents, hydrogen (H) + aluminum (Al), P, CEC, base saturation, Ca saturation, Mg saturation, and K saturation were established for tropical cover crops grown on an Oxisol.     

Tripartite symbiosis of Pisum–Glomus–Rhizobium leads to enhanced productivity,nitrogen and phosphorus economy,quality, and biofortification in garden pea in a Himalayan acid Alfisol

The present study was carried out to assess nitrogen (N) and phosphorus (P) economy, quality, and productivity of garden pea (Pisum sativum L.) through dual-inoculation of arbuscular mycorrhizal fungi (AMF) and Rhizobium in an acid Alfisol. Experiment was laid out in randomized block design replicated thrice comprising 13 treatments viz. Rhizobium along with three graded N levels (25%, 50%, and 75% soil-test-based recommended N), AMF along with three graded P levels (25%, 50%, and 75% soil-test-based recommended P), dual-inoculation of AMF and Rhizobium conjoint with four graded N and P levels (25%, 50%, 75%, and 100% soil-test-based recommended N and P), and three other treatments viz. generalized recommended NP potassium (K) dose (GRD), farmers' practice, and absolute control. The results revealed that dual-inoculation of AMF and Rhizobium enhanced the pea productivity, macronutrient (NPK) and micronutrient iron, copper, zinc, and manganese (Fe, Cu, Zn, and Mn) concentrations, and their uptake besides enhancing garden pea quality. Also, dual-inoculation of both symbionts at 75% and 100% soil-test-based N and P dose behaved statistically alike with respect to pea pod yield, NPK uptake, and quality parameters like total soluble solids (TSS) and crude protein (CP), thus indicating an economy of about 25% soil-test-based N and P dose through co-inoculation. AMF and Rhizobium dual-inoculated treatments led to enhanced TSS and CP in pea pods by 4.2% and 6.2%, respectively, over GRD, while sole application of AMF- or Rhizobium-imbedded treatments could enhance these quality parameters by 2.1% only in each case. Similarly, the highest N and P response ratio was registered in dual-inoculated treatments. Overall, dual-inoculation of AMF and Rhizobium with 75% soil-test-based N and P dose in pea can save up to 25% fertilizer N and P dose in acid Alfisol.Also, this tripartite symbiosis besides enhancing pea quality led to better bio-fortified pea seeds with micronutrients especially Fe and Zn, which can greatly curtail the widespread anemia and Zn deficiency in humans living in Himalayan acid Alfisol.