scholarly journals Soil-water physical attributes under different managements systems in the humid tropics in Maranhão

2020 ◽  
Vol 13 (9) ◽  
pp. 38
Author(s):  
J. B. Martins Filho ◽  
K. C. Cunha Meneses ◽  
A. L. Brito Filho ◽  
C. E. L. Feitosa ◽  
M. F. Farias
Keyword(s):  
Soil Moisture ◽  
Physical Properties ◽  
Soil Water ◽  
Total Porosity ◽  
Native Forest ◽  
Water Capacity ◽  
Total Soil ◽  
Randomized Design ◽  
Vertical Hydraulic Conductivity ◽  
Physical Attributes

This study was conducted to evaluate the physical properties modifications of an Oxisol under different conditions of use and management. The research was conducted at Fazenda Sítio Novo and in native forest area, respectively in the municipalities of São Benedito do Rio Preto/MA and Chapadinha/MA. The research followed a completely randomized design with 3 treatments and 4 replications, with the following uses and management: no-tillage (PD); conventional planting (CP) and native forest (MN). The following physical properties were analyzed: bulk density, porosity and soil moisture and penetration resistance at depths of 0.0-0.20 m and 0.20-0.40 m. The water properties analyzed were: basic infiltration velocity, total soil water capacity and vertical hydraulic conductivity. The soil presented higher density and low conservation of moisture in PD and PC. Native forest presented higher total porosity and higher conservation of soil moisture. Total soil water capacity was higher in MN (39.89 mm) followed by PC (25.33 mm) and PD (18.84 mm). The uses and management employed in the soils analyzed on the farm reflect the degradation of the physical properties of the soil in relation to native forest. 

scholarly journals The effects of land use and soil management on the physical properties of an Oxisol in Southeast Brazil

2014 ◽  
Vol 38 (4) ◽  
pp. 1245-1255 ◽  
Author(s):  
Getulio de Freitas Seben Junior ◽  
José Eduardo Corá ◽  
Rattan Lal
Keyword(s):  
Physical Properties ◽  
Geometric Mean ◽  
Total Porosity ◽  
Field Capacity ◽  
Soil Bulk Density ◽  
Conventional Tillage ◽  
Structural Quality ◽  
Native Forest ◽  
Tillage System ◽  
Least Limiting Water Range

Soils of the tropics are prone to a decrease in quality after conversion from native forest (FO) to a conventional tillage system (CT). However, the adoption of no-tillage (NT) and complex crop rotations may improve soil structural quality. Thus, the aim of this study was to evaluate the physical properties of an Oxisol under FO, CT, and three summer crop sequences in NT: continuous corn (NTcc), continuous soybean (NTcs), and a soybean/corn rotation (NTscr). Both NT and CT decreased soil organic carbon (SOC) content, SOC stock, water stable aggregates (WSA), geometric mean diameter (GMD), soil total porosity (TP), macroporosity (MA), and the least limiting water range (LLWR). However they increased soil bulk density (BD) and tensile strength (TS) of the aggregates when compared to soil under FO. Soil under NT had higher WSA, GMD, BD, TS and microporosty, but lower TP and MA than soil under CT. Soil under FO did not attain critical values for the LLWR, but the lower limit of the LLWR in soils under CT and NT was resistance to penetration (RP) for all values of BD, while the upper limit of field capacity was air-filled porosity for BD values greater than 1.46 (CT), 1.40 (NTscr), 1.42 (NTcc), and 1.41 (NTcs) kg dm-3. Soil under NTcc and NTcs decreased RP even with the increase in BD because of the formation of biopores. Furthermore, higher critical BD was verified under NTcc (1.62 kg dm-3) and NTcs (1.57 kg dm-3) compared to NTscr and CT (1.53 kg dm-3).

scholarly journals Physical Properties of Texturally Different Soils After Application of Biochar Substrates

2020 ◽  
Vol 66 (2) ◽  
pp. 45-55
Author(s):  
Dušan Šrank ◽  
Vladimír Šimanský
Keyword(s):  
Soil Moisture ◽  
Physical Properties ◽  
Sandy Soil ◽  
Farmyard Manure ◽  
Total Porosity ◽  
Soil Physical Properties ◽  
Climatic Conditions ◽  
Soil Amelioration ◽  
Loamy Soil ◽  
Different Soils

AbstractScientific studies show that the efficiency of biochar can be improved by its combination with other fertilisers. For this reason, fertiliser manufacturers are working to create products that combine biochar with other soil fertility enhancers suitable for different soil-climatic conditions. In this study, two types of biochar substrates (1. biochar blended with farmyard manure, and 2. biochar blended with farmyard manure as well as with digestate) at rates of 10 and 20 t/ha were applied alone or in combination with other manure and mineral fertilisers. These were added to Arenosol (sandy soil, Dolná Streda, Slovakia) and Chernozem (loamy soil, Veľké Úľany, Slovakia) to evaluate the soil physical properties to test the potential of these amendments for soil amelioration in texturally different soils. The results showed that the application of biochar substrates alone increased soil moisture, the volume of capillary pores, and decreased aeration and volume of non-capillary pores. The application of biochar substrates with mineral fertilisers increased aeration, content of water-stable macro-aggregates (WSAma), total porosity, and decreased soil moisture and the content of water-stable micro-aggregates (WSAmi) in sandy soil. In loamy soil, when compared to unfertilised control, the biochar treatments increased content of WSAma, content of dry-sieved macro-aggregates, and decreased content of WSAmi and content of dry-sieved micro-aggregates. The combination of biochar substrates together with manure had no effect on changes in the physical properties of loamy soil.

Sapwood moisture in Douglas-fir boles and seasonal changes in soil water

2007 ◽  
Vol 37 (7) ◽  
pp. 1263-1271 ◽  
Author(s):  
Peter A. Beedlow ◽  
David T. Tingey ◽  
E. Henry Lee ◽  
Donald L. Phillips ◽  
Christian P. Andersen ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Water Content ◽  
Soil Water ◽  
Seasonal Changes ◽  
Douglas Fir ◽  
Stand Age ◽  
Summer Drought ◽  
Water Capacity ◽  
The Pacific ◽  
Relative Water

Large conifers, such as Douglas-fir ( Pseudotsuga menziesii (Mirb.) Franco var. menziesii), purportedly draw on water stored in their boles during periods of summer drought. The relation of seasonal changes in soil moisture to sapwood water content was evaluated in four forest stands dominated by mature Douglas-fir along a transect from the Pacific Coast to 1200 m in the western Cascade Mountains of Oregon, USA. The sites varied in stand age, elevation, topography, and soil characteristics, including available soil water capacity. At two sites, gravimetric measures of sapwood relative water content (SRWC) were taken approximately every 4 weeks from May 2002 through July 2004; two additional sites were similarly measured from February 2003 through July 2004. Automated meteorological stations located on the sites and in adjacent open areas continuously monitored weather and soil moisture. Plant-available soil water (ASW) in the upper 0.6 m of soil reached minimum values during the summer drought and rewetted during fall and winter. Large seasonal changes in ASW did not result in corresponding changes in SRWC. Minimum SRWC was lower at sites with higher ASW. At all sites, Douglas-fir trees apparently regulate water loss to maintain consistent (±10%) bole water content throughout the year despite large changes in soil moisture.

scholarly journals Hydrophysical properties of sandy clay contaminated by petroleum hydrocarbon

2020 ◽  
Vol 27 (9) ◽  
pp. 9697-9706 ◽  
Author(s):  
Edyta Hewelke ◽  
Dariusz Gozdowski
Keyword(s):  
Soil Moisture ◽  
Physical Properties ◽  
Soil Water ◽  
Petroleum Hydrocarbon ◽  
Soil Water Potential ◽  
Water Repellency ◽  
Hydrocarbon Contamination ◽  
Soil Water Retention ◽  
Sandy Clay ◽  
Soil Retention

AbstractThe aim of the presented research was to assess the changes in hydro-physical properties of sandy clay under the influence of petroleum hydrocarbon contamination. An understanding of these changes is fundamental in the right remedial actions and for further use of soil. Laboratory tests of inherently wettable sandy clay showed that the petroleum hydrocarbon induced potential soil water repellency (SWR) of extremely repellent class at the contamination of 18 g kg−1. The relationship between soil water potential (pF) and SWR determined by the WDPT test for given hydrocarbon contamination, i.e., 6, 12, 18, 30, 100 g kg−1, showed that the critical soil moisture value (CSMC) corresponds to the pF = 1.0 ÷ 1.5. Soil retention characteristic (pF) showed that an increase in hydrocarbon contamination from 0 to 100 g kg−1 caused a reduction of total available water for plants from about 0.19 to 0.06 cm cm−3. At the same time, in the pF = 1.5 ÷ 2.0 range, intensive soil pore drainage was observed. Statistically, significant effect of hydrocarbon contamination and soil moisture potential on SWR was found. Soil hydrophobicity limits the addition of soil retention, because a significant part of the precipitation can be transformed by surface runoff. The carried out tests showed that at a hydrocarbon contamination of 30 g kg−1, total rainfall amount 14 mm with an intensity of 2 mm h−1 was transformed into a surface drain in approx. 40%. The conducted studies demonstrate the adverse impact of hydrocarbon contamination on the soil’s hydro-physical properties. The soil water retention reduction and launching of the surface outflow, as a result of limiting the water penetration process resulting from SWR, change the agrohydrological conditions of the contaminated area. It can result as the imbalance of the flow of energy and matter in the ecosystem. The scenarios of environmental effects, among others, depend on the type of soil, the degree of its pollution, the type of ecosystem, and supporting activities undertaken by man. It should be taken into account that the increasing frequency of drought occurrence associated with climate change is conducive to the phenomenon of SWR regardless of the reasons for its occurrence.

scholarly journals Soil physical properties and grape yield influenced by cover crops and management systems

2013 ◽  
Vol 37 (5) ◽  
pp. 1352-1360 ◽  
Author(s):  
Jaqueline Dalla Rosa ◽  
Alvaro Luiz Mafra ◽  
João Carlos Medeiros ◽  
Jackson Adriano Albuquerque ◽  
Davi José Miquelluti ◽  
...  
Keyword(s):  
Physical Properties ◽  
Cover Crops ◽  
Soil Layer ◽  
Aggregate Stability ◽  
Total Porosity ◽  
Soil Physical Properties ◽  
Management Systems ◽  
Native Forest ◽  
Crop Species ◽  
Grape Yield

The use of cover crops in vineyards is a conservation practice with the purpose of reducing soil erosion and improving the soil physical quality. The objective of this study was to evaluate cover crop species and management systems on soil physical properties and grape yield. The experiment was carried out in Bento Gonçalves, RS, Southern Brazil, on a Haplic Cambisol, in a vineyard established in 1989, using White and Rose Niagara grape (Vitis labrusca L.) in a horizontal, overhead trellis system. The treatments were established in 2002, consisting of three cover crops: spontaneous species (SS), black oat (Avena strigosa Schreb) (BO), and a mixture of white clover (Trifolium repens L.), red clover (Trifolium pratense L.) and annual rye-grass (Lolium multiflorum L.) (MC). Two management systems were applied: desiccation with herbicide (D) and mechanical mowing (M). Soil under a native forest (NF) area was collected as a reference. The experimental design consisted of completely randomized blocks, with three replications. The soil physical properties in the vine rows were not influenced by cover crops and were similar to the native forest, with good quality of the soil structure. In the inter-rows, however, there was a reduction in biopores, macroporosity, total porosity and an increase in soil density, related to the compaction of the surface soil layer. The M system increased soil aggregate stability compared to the D system. The treatments affected grapevine yield only in years with excess or irregular rainfall.

In a native pasture, landscape properties influence soil moisture more than grazing management

2017 ◽  
Vol 57 (9) ◽  
pp. 1799 ◽  
Author(s):  
D. C. Mitchell ◽  
W. B. Badgery ◽  
P. Cranney ◽  
K. Broadfoot ◽  
S. Priest ◽  
...  
Keyword(s):  
Soil Moisture ◽  
Soil Water ◽  
Grazing Management ◽  
Near Surface ◽  
Water Capacity ◽  
Available Water ◽  
Available Water Capacity ◽  
High Production ◽  
Plant Available Water ◽  
Production Zone

It has been proposed that changes to grazing systems, from continuous to rotational grazing, alter the pasture mass and composition, which are reflected in changes to stored soil water. Additionally, in highly variable landscapes, determining whether the variation in soil water is due to the inherent landscape properties rather than the imposed grazing management has long been a contentious argument. To address this question, soil moisture was measured across a highly variable landscape under three differing grazing treatments (1-, 4- and 20-paddock systems). From the soil-water measurements, plant-available water and plant-available water capacity were determined. Different production zones (high, medium and low) were identified in the landscape by visually estimating green herbage mass in late spring. There were no observed differences in the measured plant-available water capacity across the grazing treatments; however, significant differences occurred in plant-available water capacity across the three production zones (high-production zone, 114 mm; medium-production zone, 102 mm; low-production zone, 88 mm) within the study period. There appears to be a trend between the plant-available water capacity and near-surface gravel content as measured in production zones. The high production zones held more plant-available water than did the low production zones, enabling more biomass and longer pasture growth during spring and autumn. The plant-available water in the low production zones significantly decreased with time. In all, 22 of the 50 soil-moisture monitoring locations displayed high temporal stability and were identified as being catchment-average soil water-content monitoring locations. A majority of these locations occurred in the medium production zone, demonstrating that representative soil moisture can be measured in these landscapes.

scholarly journals Physical properties of a rhodic haplustox under two sugarcane harvesting systems

2010 ◽  
Vol 34 (6) ◽  
pp. 1803-1809 ◽  
Author(s):  
Walquíria Machado ◽  
Tiago Santos Telles ◽  
João Tavares Filho ◽  
Maria de Fátima Guimarães ◽  
Grace Bungenstab Alves ◽  
...  
Keyword(s):  
Physical Properties ◽  
Bulk Density ◽  
Weighted Average ◽  
Aggregate Stability ◽  
Total Porosity ◽  
Average Diameter ◽  
Penetration Resistance ◽  
Soil Bulk Density ◽  
Native Forest ◽  
Harvesting Systems

This study had the purpose of evaluating the effects of two management types of sugarcane: harvesting of burnt cane (BCH) and mechanized harvesting of unburnt green cane (MCH), on some soil physical properties of a dystrophic Rhodic Haplustox. The data were then compared with results for the same soil type under native forest. A completely randomized design was used, with three treatments and 20 replications. The following characteristics were determined: organic matter, aggregate stability, soil bulk density, and porosity at depths of 0-0.20 m and soil penetration resistance. After 15 years of cultivation, there were some alterations in the soil under cane burnt before harvesting, evidenced by a drop in the weighted average diameter of stable aggregates in water and increased soil bulk density. Significant changes were also detected in total porosity and pore distribution under both harvesting systems. Critical values for penetration resistance were observed in the area under mechanized sugar cane harvesting, with a value of 4.5 MPa in the 40-55 cm layer. This value is considered high and could indicate compaction and restriction of root growth. Soil properties under the green cane (unburned) management system were closest to those of the soil under native forest.

scholarly journals Comparison of the physical properties of soils belonging to different reference soil groups

2020 ◽  
Vol 16 (No. 1) ◽  
pp. 29-38
Author(s):  
Jan Vopravil ◽  
Pavel Formánek ◽  
Tomáš Khel
Keyword(s):  
Physical Properties ◽  
Bulk Density ◽  
Particle Density ◽  
Total Porosity ◽  
Capillary Water ◽  
Water Capacity ◽  
Available Water Capacity ◽  
Permanent Wilting Point ◽  
Wilting Point ◽  
Soil Groups

Soil properties can be influenced by long-term agricultural management practices as described in pedological literature. In this study, selected physical properties (particle density and bulk density, total porosity, maximum capillary water capacity, minimum air capacity, field capacity, permanent wilting point and available water capacity) of topsoils from different reference soil groups (Cambisols, Luvisols, Fluvisols, Chernozems and Phaeozems, Leptosols, Stagnosols and Gleysols) were sampled and analysed in the years 2016–2017. The topsoil samples were taken from points of so-called S (specific) soil pits to be sampled from the General Soil Survey of Agricultural Soils (GSSAS) which was accomplished in the years 1961–1970. In addition, some of the properties were also compared with those measured during the GSSAS. Recognising the properties, only the particle density, the maximum capillary water capacity, the permanent wilting point and the available water capacity of the topsoil of the individual soil groups were statistically significantly (P < 0.05) different. A comparison of the physical properties with those analysed after more than 40 years was performed, the bulk density increased and the total porosity decreased in the topsoil of the major part of the studied soil groups.

Survival of Chlamydospores of Phytophthora cinnamomi in Several Non-Sterile, Host-Free Forest Soils and Gravels at Different Soil Water Potentials

1979 ◽  
Vol 27 (1) ◽  
pp. 1 ◽  
Author(s):  
G Weste ◽  
K Vithanage
Keyword(s):  
Soil Moisture ◽  
Soil Water ◽  
Phytophthora Cinnamomi ◽  
Matter Content ◽  
Soil Types ◽  
Native Forest ◽  
Sterile Soil ◽  
Water Potentials ◽  
Chlamydospore Formation ◽  
Disease Free

Chlamydospore survival was investigated for six soil types, collected from disease-free areas of native forest in Victoria, in 50-g packs of non-sterile, unamended soils and gravels at five different matric soil water potentials ( ψ ). No chlamydospores survived in gravel free from OM, and only one chlamydospore survived at ψ -3000 kPa. In other packs the numbers of chlamydospores declined for 2 months then increased markedly at 4-6 months. Many chlamydospores remained viable for 8 months and some for 10 months despite the use of non-sterile soil and the absence of hosts. Maximum numbers survived in gravel from the Brisbane Ranges 6 and 8 months after inoculation at ψ -500 kPa. Decreasing soil moisture appeared to stimulate chlamydospore formation while a low rganic matter content and small numbers of microorganisms increased survival.

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