scholarly journals TO SOLVE THE PROBLEMS OF DIAGNOSING THE GROSS RESOURCE OF LICORICE ROOT AND ITS EXTRACTION IN THE VOLGA-AKHTUBA FLOODPLAIN

2021 ◽  
Vol 16 (4) ◽  
pp. 42-47
Author(s):  
Vitaliy Mamin ◽  
Tat'yana Koshkarova ◽  
Ekaterina Zinchenko ◽  
Lyubov' Vronskaya ◽  
Natal'ya Kruglyakova
Keyword(s):  
Root System ◽  
Sandy Loam ◽  
Soil Layer ◽  
Licorice Root ◽  
Root Mass ◽  
Alluvial Deposits ◽  
Ecological Features ◽  
Subsurface Waters ◽  
Physical And Chemical ◽  
Alluvial Meadow

The article reflects the results of many years of research on the study of the root system of naked licorice (Glycyrrhiza glаbra L.). The formation of this valuable plant occupies significant areas of the Volga-Akhtuba floodplain. The work was carried out in order to establish the regularities of the formation and accumulation of roots in local populations of licorice in order to diagnose their reserves with subsequent scientific substantiation of technological regulations for the industrial production of licorice, which guarantee self-restoration of cenopopulations. Based on the totality of morphological and ecological features, the diversity of adaptability of architectonics, the root system of licorice can be regarded as ecologically universal and, in some respects, unique. The multivariance of its structure for a number of typical habitats of this plant is explained by the influence of different regimes of surface waters during floods and subsurface waters during the growing season, in conditions of a wide variety of alluvial deposits along the profile of the soil aeration zone, their physical and chemical characteristics. The floodplain formation of naked licorice includes a large number of communities of various species composition, which, with varying degrees of its participation, are among the seven most frequently encountered associations. The most productive are clean malt houses formed in the central (insular) part of the lower floodplain and delta under conditions of annual flood moistening of soils. Licorice acquires the most intensive productive development, settling on non-saline floodplain alluvial meadow and meadow dark-colored granular soils of light granulometric composition, as well as on alluvial meadow sandy loam soils formed on middle flood relief elements. In these habitats, the root mass (total, wet) in the soil layer of 0.40 m can reach 22 ... 25 tons per hectare in some areas. Most often, the root mass of licorice naked along the soil profile is distributed as follows: 90% of all roots and rhizomes - in a layer of 1.0 ... 1.2 m, including 60% - in a layer of 0 ... 0.3 m, 20% - in layer 0.3 ... 0.5 m

Directed formation of fertility of soils in Non-Chernozem region, taking into account the potential capabilities of arable crops

2020 ◽  
pp. 48-53
Author(s):  
Vladimir Maximenko ◽  
Tatyana Volchkova ◽  
Snezana Menshikova
Keyword(s):  
Root System ◽  
Crop Production ◽  
Soil Layer ◽  
Chemical Properties ◽  
Subsequent Treatment ◽  
Reclaimed Soil ◽  
Deep Layers ◽  
Different Depths ◽  
Favorable Conditions ◽  
Physical And Chemical

The article considers the possibility of directed formation of soil fertility in the conditions of crop production by increasing the efficiency of accumulation of incoming solar energy by crops. The effect is provided by deep volumetric loosening with one-time intra-soil introduction of meliorant, cultivation of crop-meliorant and subsequent treatment of different depths of the reclaimed soil layer for agricultural crops rotation. Given that the root system of plants affects the physical and chemical properties of the soil, its deeper placement contributes to the enrichment of deep layers soil of nutrients. Directed formation of the root system in the likeness of its natural development in favorable conditions of structural addition provides natural deposition in its layers of elements available for subsequent crops.

scholarly journals Assessment of Seasonal Variability in Soil Nutrients and Its Impact on Soil Quality under Different Land Use Systems of Lower Shiwalik Foothills of Himalaya, India

2021 ◽  
Vol 13 (3) ◽  
pp. 1398
Author(s):  
Tavjot Kaur ◽  
Simerpreet Kaur Sehgal ◽  
Satnam Singh ◽  
Sandeep Sharma ◽  
Salwinder Singh Dhaliwal ◽  
...  
Keyword(s):  
Land Use ◽  
Soil Quality ◽  
Surface Soil ◽  
Sandy Loam ◽  
Monsoon Season ◽  
Soil Layer ◽  
Seasonal Effects ◽  
Land Use Systems ◽  
Post Monsoon ◽  
Significant Difference

The present study was conducted to investigate the seasonal effects of five land use systems (LUSs), i.e., wheat–rice (Triticum aestivum—Oryza sativa) system, sugarcane (Saccharum officinarum), orange (Citrus sinensis) orchard, safeda (Eucalyptus globules) forest, and grassland, on soil quality and nutrient status in the lower Satluj basin of the Shiwalik foothills Himalaya, India. Samples were analyzed for assessment of physico-chemical properties at four soil depths, viz., 0–15, 15–30, 30–45, and 45–60 cm. A total of 120 soil samples were collected in both the seasons. Soil texture was found to be sandy loam and slightly alkaline in nature. The relative trend of soil organic carbon (SOC), macro- and micro-nutrient content for the five LUSs was forest > orchard > grassland > wheat–rice > sugarcane, in the pre- and post-monsoon seasons. SOC was highly correlated with macronutrients and micronutrients, whereas SOC was negatively correlated with soil pH (r = −0.818). The surface soil layer (0–15 cm) had a significantly higher content of SOC, and macro- and micro-nutrients compared to the sub-surface soil layers, due to the presence of more organic content in the soil surface layer. Tukey’s multiple comparison test was applied to assess significant difference (p < 0.05) among the five LUSs at four soil depths in both the seasons. Principle component analysis (PCA) identified that SOC and electrical conductivity (EC) were the most contributing soil indicators among the different land use systems, and that the post-monsoon season had better soil quality compared to the pre-monsoon season. These indicators helped in the assessment of soil health and fertility, and to monitor degraded agroecosystems for future soil conservation.

scholarly journals Biochar induced improvement in root system architecture enhances nutrient assimilation by cotton plant seedlings

2021 ◽  
Vol 21 (1) ◽  
Author(s):  
Lei Feng ◽  
Wanli Xu ◽  
Guangmu Tang ◽  
Meiying Gu ◽  
Zengchao Geng
Keyword(s):  
Root System ◽  
System Architecture ◽  
Fine Roots ◽  
Nitrogen Assimilation ◽  
Surface Soil ◽  
Soil Layer ◽  
Root System Architecture ◽  
Seedling Stage ◽  
Agronomic Efficiency ◽  
Surface Soil Layer

Abstract Background Raising nitrogen use efficiency of crops by improving root system architecture is highly essential not only to reduce costs of agricultural production but also to mitigate climate change. The physiological mechanisms of how biochar affects nitrogen assimilation by crop seedlings have not been well elucidated. Results Here, we report changes in root system architecture, activities of the key enzymes involved in nitrogen assimilation, and cytokinin (CTK) at the seedling stage of cotton with reduced urea usage and biochar application at different soil layers (0–10 cm and 10–20 cm). Active root absorption area, fresh weight, and nitrogen agronomic efficiency increased significantly when urea usage was reduced by 25% and biochar was applied in the surface soil layer. Glutamine oxoglutarate amino transferase (GOGAT) activity was closely related to the application depth of urea/biochar, and it increased when urea/biochar was applied in the 0–10 cm layer. Glutamic-pyruvic transaminase activity (GPT) increased significantly as well. Nitrate reductase (NR) activity was stimulated by CTK in the very fine roots but inhibited in the fine roots. In addition, AMT1;1, gdh3, and gdh2 were significantly up-regulated in the very fine roots when urea usage was reduced by 25% and biochar was applied. Conclusion Nitrogen assimilation efficiency was significantly affected when urea usage was reduced by 25% and biochar was applied in the surface soil layer at the seedling stage of cotton. The co-expression of gdh3 and gdh2 in the fine roots increased nitrogen agronomic efficiency. The synergistic expression of the ammonium transporter gene and gdh3 suggests that biochar may be beneficial to amino acid metabolism.

Towards the consideration of soil-root resistances in root water uptake models with macroscopic representations of hydraulic root architecture

2021 ◽  
Author(s):  
Jan Vanderborght ◽  
Valentin Couvreur ◽  
Felicien Meunier ◽  
Andrea Schnepf ◽  
Harry Vereecken ◽  
...  
Keyword(s):  
Root System ◽  
Soil Water ◽  
Water Uptake ◽  
Root Distribution ◽  
Root Architecture ◽  
Soil Layer ◽  
Root Water Uptake ◽  
Hydraulic Architecture ◽  
Root Segments ◽  
Soil Volume

&lt;p&gt;Plant water uptake from soil is an important component of terrestrial water cycle with strong links to the carbon cycle and the land surface energy budget. To simulate the relation between soil water content, root distribution, and root water uptake, models should represent the hydraulics of the soil-root system and describe the flow from the soil towards root segments and within the 3D root system architecture according to hydraulic principles. We have recently demonstrated how macroscopic relations that describe the lumped water uptake by all root segments in a certain soil volume, e.g. in a thin horizontal soil layer in which soil water potentials are uniform, can be derived from the hydraulic properties of the 3D root architecture. The flow equations within the root system can be scaled up exactly and the total root water uptake from a soil volume depends on only two macroscopic characteristics of the root system: the root system conductance, K&lt;sub&gt;rs&lt;/sub&gt;, and the uptake distribution from the soil when soil water potentials in the soil are uniform, &lt;strong&gt;SUF&lt;/strong&gt;. When a simple root hydraulic architecture was assumed, these two characteristics were sufficient to describe root water uptake from profiles with a non-uniform water distribution. This simplification gave accurate results when root characteristics were calculated directly from the root hydraulic architecture. In a next step, we investigate how the resistance to flow in the soil surrounding the root can be considered in a macroscopic root water uptake model. We specifically investigate whether the macroscopic representation of the flow in the root architecture, which predicts an effective xylem water potential at a certain soil depth, can be coupled with a model that describes the transfer from the soil to the root using a simplified representation of the root distribution in a certain soil layer, i.e. assuming a uniform root distribution.&lt;/p&gt;

scholarly journals Physical and chemical attributes of archaeological soils developed from shell middens in the Região dos Lagos, Rio de Janeiro, Brazil

2011 ◽  
Vol 35 (4) ◽  
pp. 1100-1111 ◽  
Author(s):  
Guilherme Resende Corrêa ◽  
Carlos Ernesto G.R Schaefer ◽  
Vander de Freitas Melo ◽  
Kleberson Worslley de Souza ◽  
João Carlos Ker ◽  
...  
Keyword(s):  
Sandy Loam ◽  
Chemical Properties ◽  
Brazilian Coast ◽  
High Fertility ◽  
Physical Analysis ◽  
Shell Middens ◽  
Organic C ◽  
Chemical Attributes ◽  
Região Dos Lagos ◽  
Physical And Chemical

In prehistoric times, innumerous shell middens, called "sambaquis", consisting mainly of remains of marine organisms, were built along the Brazilian coast. Although the scientific community took interest in these anthropic formations, especially since the nineteenth century, their pedological context is still poorly understood. The purpose of this study was to characterize and identify the physical and chemical changes induced by soil-forming processes, as well as to compare the morphology of shell midden soils with other, already described, anthropogenic soils of Brazil. Four soil profiles developed from shell middens in the Região dos Lagos - RJ were morphologically described and the physical and chemical properties determined. The chemical analysis showed that Ca, Mn, Mg, and particularly P and Zn are indicators of anthropic horizons of midden soils, as in the Amazon Dark Earths (Terras Pretas de Índio). After the deposition of P-rich material, P reaction and leaching can mask or disturb the evidence of in situ man-made strata, but mineralogical and chemical studies of phosphate forms can elucidate the apparent complexity. Lower phosphate-rich strata without direct anthropic inputs indicate P leaching and precipitation in secondary forms. The total and bioavailable contents of Ca, Mg, Zn, Mn, Cu, P, and organic C of midden soils were much higher than of regional soils without influence of ancient human settlements, demonstrating that the high fertility persisted for long periods, at some sites for more than 4000 years. The physical analysis showed that wind-blown sand contributed significantly to increase the sand fraction in the analyzed soils (texture classes sand, sandy loam and sandy clay loam) and that the aeolian sand accumulation occurred simultaneously with the midden formation.

scholarly journals Synergy Between a Shallow Root System With a DRO1 Homologue and Localized P Application Improves Rice P Uptake 

2021 ◽  
Author(s):  
Aung Zaw Oo ◽  
YASUHIRO TSUJIMOTO ◽  
Mana Mukai ◽  
Tomohiro Nishigaki ◽  
Toshiyuki Takai ◽  
...  
Keyword(s):  
Root System ◽  
Crop Production ◽  
Soil Layer ◽  
P Uptake ◽  
Ore Deposits ◽  
Root Surface Area ◽  
Genetic Traits ◽  
P Use Efficiency ◽  
Use Efficiency ◽  
P Application

Abstract Improved phosphorus (P) use efficiency for crop production is needed given the depleting phosphorus ore deposits and increasing ecological concerns about its excessive use. Root system architecture (RSA) is important in efficiently capturing immobile P in soils, while agronomically, localized P application near the roots is a potential approach to address this issue. However, the interaction between genetic traits of RSA and localized P application has been little understood. Near-isogenic lines (NILs) and their parent of rice (qsor1-NIL, Dro1-NIL, and IR64, with shallow, deep, and intermediate root growth angles (RGA), respectively) were grown in flooded pots after placing P near the roots at transplanting (P-dipping). The experiment identified that the P-dipping created an available P hotspot at the soil surface; the qsor1-NIL had the greatest root biomass and root surface area in the 0–3 cm soil layer despite no genotype differences in total values; the qsor1-NIL had significantly greater biomass and P uptake than the other genotypes in the P-dipping. The superior surface root development of qsor1-NIL could have facilitated P uptakes from the P hotspot, implying that P-use efficiency in crop production can be further increased by combining genetic traits of RSA and localized P application.

scholarly journals Soil water extraction by roots and Kc for the coffee crop

2009 ◽  
Vol 13 (3) ◽  
pp. 257-261 ◽  
Author(s):  
Adriana L. da Silva ◽  
Isabeli P. Bruno ◽  
Klaus Reichardt ◽  
Osny O. S. Bacchi ◽  
Durval Dourado-Neto ◽  
...  
Keyword(s):  
Root System ◽  
Soil Water ◽  
Dry Matter ◽  
Soil Layer ◽  
Water Extraction ◽  
Area Index ◽  
Direct Measurements ◽  
Top Soil ◽  
Soil Water Extraction ◽  
Crop Coefficients

Basic information for a rational soil-water management of the coffee crop is still insufficient, particularly under irrigated conditions. Of great importance for the estimation of water requirements of coffee crops are their root distribuition and evapotranspiration crop coefficients. This study compares soil water extraction by roots of coffee plants of the variety "Catuaí Vermelho" (IAC-44), grown in Piracicaba, SP, Brazil, 3 to 5 years old, with direct measurements of root dry matter, showing a good agreement between both approaches, and confirming that most of the root system is distributed in the top soil layer (0-0.3 m) and that less than 10% of the root system reaches depths greater than 1.0 m. Calculated evapotranspiration crop coefficients are in agreement with those found in the literature, with an average of 1.1, independent of shoot dry matter, plant height and leaf area index.

scholarly journals Stabilization of organic material from soils and soil-like bodies in the Lena River Delta (13C-NMR spectroscopy analysis)

2020 ◽  
Vol 10 ◽  
Author(s):  
Vyacheslav Polyakov ◽  
Evgeny Abakumov
Keyword(s):  
Nmr Spectroscopy ◽  
Humic Acids ◽  
Soil Layer ◽  
13C Nmr Spectroscopy ◽  
River Delta ◽  
The Arctic ◽  
Polar Regions ◽  
Alluvial Deposits ◽  
Lena River ◽  
Lena River Delta

The Arctic ecosystem has a huge reservoir of soil organic carbon stored in permafrost-affected soils and biosediments. During the short vegetation season, humification and mineralization processes in the active soil layer result in the formation of specific soil organic substances – humic substances. Humic acids are high molecular, specific, thermodynamically stable macromolecules. The study was conducted in the Lena River Delta, the largest river delta located in the Arctic. Cryosol-type soils on alluvial deposits of the river form an area of about 45 thousand km<sup>2</sup> under permafrost conditions. The vegetation cover is represented by moss-lichen communities with the presence of <em>Salix glauca</em> in the flooded areas, as well as <em>Betula nana</em> in the areas not subject to flooding. The paper presents the elemental and molecular composition of humic acids isolated from soils, integral indicators of humification (stabilization) of organic matter in the soils of the Lena River Delta. The study was conducted using the <sup>13</sup>C (CP/MAS) NMR spectroscopy method. In the work, it was revealed that up to 33% of aromatic and up to 15% COOR fragments are accumulated in humic acids. The AR/AL ratio ranged from 0.69 to 0.89. The studied soils are variants of modern soil formation (not subjected to alluvial processes) and soil-like bodies that melted from the IC of the river delta. A relatively high degree of condensation of humic acid macromolecules in comparison with other polar regions of the Arctic and Antarctic was noted.

Root depth of native and sown perennial grass-based pastures, North-West Slopes, New South Wales. 1. Estimates from cores and effects of grazing treatments

2006 ◽  
Vol 46 (3) ◽  
pp. 337 ◽  
Author(s):  
G. M. Lodge ◽  
S. R. Murphy
Keyword(s):  
Root Length ◽  
Root Length Density ◽  
Mass Density ◽  
Perennial Grass ◽  
Soil Layer ◽  
Volume Density ◽  
Root Mass ◽  
Root Depth ◽  
Root Volume ◽  
Native Pasture

Studies were undertaken on native and sown perennial grass-based pastures as part of the Sustainable Grazing Systems National Experiment to estimate root depth and describe root distribution in these pastures. Samples from soil cores (0–210 cm maximum sampling depth) taken in 1997 (before grazing treatments were imposed) and 4 years later in spring 2001 were used to examine the effects of different grazing regimes on root length density (cm/cm3), root mass density (mg/cm3), root volume density (cm3/cm3), and diameter (mm) at each of 3 sites. In spring 1997, mean maximum root depth was 107 cm for a native perennial grass pasture near Barraba and 74 cm for a pasture sown with phalaris (Phalaris aquatica) and subterranean clover (Trifolium subterraneum) near Nundle, with values being lower for a native pasture near Manilla (65 cm for a Brown Vertosol and 97 cm for a Red Chromosol). For all pasture types, >20% of root mass density, root length density or root volume density was in the 0–5 cm soil layer and >60% was at a depth of 0–30 cm. At all sites, mean total root mass was around 1000 kg DM/ha. After 4 years of grazing (spring 2001) there were relatively few significant effects of grazing treatment on root length density, root mass density, root volume density, or root diameter. Effects that were significant mostly occurred at 0–5 cm for the native pastures and 0–50 cm for the sown pasture. For the Barraba native pasture, root length, volume and mass densities (0–5 cm) were higher (P<0.05) in the continuously grazed, low stocking rate treatment compared with all other treatments. Similarly, for the Manilla native pasture, root length density was higher (P<0.05) in this treatment at soil depths of 0–5 and >5–10 cm compared with all other treatments. In contrast, for the Nundle sown pasture, root length density (0–5 cm) was lowest (P<0.05) in 2 continuously grazed treatments compared with those that were strategically grazed in autumn and spring.

Phosphorus dynamics in shallow subsurface waters in an uncut and cut subcatchment of a lake on the Boreal Plain

2000 ◽  
Vol 57 (S2) ◽  
pp. 60-72 ◽  
Author(s):  
J E Evans ◽  
E E Prepas ◽  
K J Devito ◽  
B G Kotak
Keyword(s):  
Water Samples ◽  
Soil Layer ◽  
Organic Layer ◽  
Mineral Layer ◽  
Near Surface ◽  
Organic C ◽  
Shallow Subsurface ◽  
Phosphorus Dynamics ◽  
Subsurface Waters ◽  
Composite Samples

Phosphorus dynamics in shallow subsurface waters (<2.5 m depth) were studied in harvested and unharvested subcatchments of a Boreal Plain lake. The organic soil layer was underlain by discontinuous layers of sand and clay glacial till. Total dissolved P (TDP) concentrations (6-798 µg·L-1) of discrete water samples from mineral layers (0.9-2.5 m deep) generally decreased with depth, were negatively related to Ca (rs < -0.7), and were lower in clay. When the groundwater table rose and saturated the organic layer, TDP concentrations increased in the composite (organic mineral layer) but not in the discrete (mineral layer) water samples, indicating that elevated TDP concentrations originate from the near-surface organic layer. TDP concentrations in composite samples were negatively correlated with water table depth (rs = -0.6) and were positively correlated with transmissivity (rs = 0.7) and dissolved organic C concentration (rs > 0.6). In the riparian buffer zone of the harvested subcatchment, TDP concentrations of composite samples decreased during high runoff, but these values remained higher than concentrations in the unharvested subcatchment. However, surface topography and variable depth to confining clay layers resulted in higher groundwater tables in the harvested subcatchment, especially in the cut area. Mean daily TDP export coefficients were similar between the unharvested (14 µg·m-2) and harvested (12 µg·m-2) subcatchments.

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