scholarly journals Analysis of The Relationship Between Microbial Activities In Humus Soil Towards Infiltration Rate for Fertility Improvement With Biosoildam Technology for Corn Plantation

2021 ◽  
Vol 6 (10) ◽  
pp. 5251
Author(s):  
Nugroho Widiasmadi
Keyword(s):  
Infiltration Rate ◽  
Microbial Activities ◽  
The Relationship ◽  
Humus Soil

scholarly journals Root mass may affect soil water infiltration more strongly than the incorporated residue

F1000Research ◽  
2019 ◽  
Vol 7 ◽  
pp. 1523 ◽  
Author(s):  
Masato Oda ◽  
Burhanuddin Rasyid ◽  
Hide Omae
Keyword(s):  
Soil Erosion ◽  
Soil Water ◽  
Crop Residue ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Root Mass ◽  
Soil Water Infiltration ◽  
Residue Incorporation ◽  
Crop Residue Incorporation ◽  
The Relationship

Crop residue incorporation increases stable soil pores and soil water infiltration and reduces surface water runoff and soil erosion. However, few studies have examined the relationship between crop residue incorporation and water infiltration. A previous study showed that water infiltration increases depending on the quantity of applied wheat straw. In this study, we examined whether the relationship is applicable to different crop residues in a crop rotation. We grew corn, rose grass, and okra in crop rotation under plastic film houses and measured the water infiltration rate at the time of ridge making. A strong correlation was found between the quantity of applied residue and the soil water infiltration rate (r = 0.953), although there are outliers in the case of no prior crop. However, aboveground biomass of the prior crop showed a stronger correlation with water infiltration rate (r = 0.965), without outliers. Previous studies have revealed the exponential relation between plant root mass and soil erosion. Our data also show a positive relationship between resistance to erosion and root mass when assuming that aboveground biomass is proportional to the underground biomass. The result also showed that the effect of the prior crop root mass disappears within the next crop period. Our results indicate that maintaining a large root biomass is crucial for reducing soil erosion.

scholarly journals Soil Improvement & Conservation Based on Biosoildam Integrated Smart Ecofarming Technology (Applied in Java Alluvial Land & Arid Region in East Indonesia)

2020 ◽  
Vol 5 (9) ◽  
pp. 599-608
Author(s):  
Nugroho Widiasmadi
Keyword(s):  
Soil Temperature ◽  
Microbial Activity ◽  
Infiltration Rate ◽  
Temperature Sensors ◽  
North Coast ◽  
Digital Information ◽  
Livestock Waste ◽  
Electrolyte Conductivity ◽  
Conductivity Sensor ◽  
The Relationship

Biosoildam a technology that combines agricultural and environmental activities (water & soil conservation) based on IOT. This analysis aims to improve alluvial agricultural lands by analyzing the relationship between microbial activity on acidity and the infiltration rate for alluvial lands that widely spread on the north coast of Java with Biosoildam Technology. Microbial activity as a biological agent / biofertilizer of slurry biomass decomposition taken from the livestock center and soil conditioning will affect soil electrolyte conductivity (EC). Other variables use the humidity and soil temperature parameters to control the relationship. Integrated Ecofarming where harvest straw for feed and livestock waste for fertilizer in micobial decomposting process is a cost-effective method that can improve soil quickly and measurably. The research took place from January to July 2018 on the red onion farms in Nganjuk Regency. The tools used include Double Ring Infiltrometer for measuring the infiltration rate at three radial distances from the centre of the microbial hole (biohole), microcontroller & wifi, electrolyte conductivity sensor as the soil fertility indication, pH meter for measuring soil acidity, and humidity and soil temperature sensors. The real-time information on soil paramaters is obtained through analogue inputs from EC, pH, humidity and temperature sensors, converted into digital information data by a microcontroller which later sent via wifi. Sensors are spreadly placed with radius A= 1,5 m ;B= 2 m ; C= 3m. Average Result : infiltration rate =40cm/h EC=1100 M=45 % T=25°C pH=6,5.

scholarly journals INFLUÊNCIA DAS CARACTERÍSTICAS AMBIENTAIS E DOS INFLUÊNCIA DAS CARACTERÍSTICAS AMBIENTAIS E DOS ATRIBUTOS DO SOLO NA INFILTRAÇÃO DA ÁGUA EM ÁREA URBANAATRIBUTOS DO SOLO NA INFILTRAÇÃO DA ÁGUA EM ÁREA URBANA

2020 ◽  
Vol 38 (4) ◽  
pp. 1029-1038
Author(s):  
Jéssyca Stanieski de SOUZA ◽  
Isabel Kaufmann de ALMEIDA ◽  
Glauber Altrão CARVALHO ◽  
Teodorico ALVES SOBRINHO ◽  
Cláudia Gonçalves Vianna BACCHI
Keyword(s):  
Physical Properties ◽  
Overland Flow ◽  
Infiltration Rate ◽  
Soil Physical Properties ◽  
Capital City ◽  
Soil Infiltration ◽  
Environmental Characteristics ◽  
Mato Grosso ◽  
Flow Simulator ◽  
The Relationship

This study investigated the influence of the environmental characteristics and soil properties on the soil infiltration rate in urban permeable area. The experiments were conducted at nine sampling points located in the urban perimeter of Campo Grande, capital city of Mato Grosso do Sul State, in the Brazilian Midwest. The infiltration rates were determined using a portable integrated rainfall and overland flow simulator. Each experiment was repeated three times, and a total of twenty-seven plots were collected. At the same time, environmental characteristics and soil physical properties, that may affect infiltration rate, were also evaluated. The relationship between the infiltration rate, the environmental plot characteristics and the soil physical properties was verified using a linear correlation matrix.

scholarly journals Effect of Slope on Infiltration Capacity and Erosion of Mount Merapi Slope Materials

2020 ◽  
Vol 1000 (1000) ◽  
Author(s):  
Adam Pamudji Rahardjo
Keyword(s):  
Surface Runoff ◽  
Erosion Rate ◽  
Soil Surface ◽  
Infiltration Rate ◽  
Infiltration Capacity ◽  
Erosion Rates ◽  
Slope Steepness ◽  
Balance Principle ◽  
Exponential Equations ◽  
The Relationship

 Infiltration which occurs on slope has a specific behavior that can be parameterized. One of the reasons is because the slope generates less ponding on the sloping soil surface. This condition affects infiltration rate and surface runoff proportion of water from any kind of rainfall distribution in time. Since surface runoff tends to be higher, erosion rate is also to be higher on slope. The slope steepness is the most important parameter of a slope. In this study, the effect of slope steepness on infiltration capacity and erosion rate of Mount Merapi bare slope material were tested in a laboratory using rainfall simulator. Three values of slope steepness of 36%, 47%, and 58% were used. The rainfall intensity was set constant and was found has rate of 116,312 mm/hour. The infiltration rate was measured by volumetric balance principle and the erosion rates were measured by collecting the eroded grains at the downstream end tank. Infiltration rate was evaluated by using Horton method and the average erosion were analyzed from the eroded grain data for each test. After fitting the recorded infiltration rate data to the Horton equation, the infiltration capacity was obtained. The results were the relationship between slope steepness and the affected the infiltration capacity and erosion for each test. Infiltration capacity is found to increase and the decrease with the increase of slope steepness while erosion rate is found to increase on the steeper slope. The increase of erosion range is between 15% to 33% for each 1o increase of slope steepness. In addition, polynomial and exponential equations were developed to express the relationship between slope steepness and infiltration capacity and also the erosion rate.

scholarly journals Modelling flood hazard at Paratrechos/Peritsi stream, Naxos Island (Cyclades, Greece)

2018 ◽  
Vol 20 (1) ◽  
pp. 123-129
Author(s):  
Niki EVELPIDOU ◽  
Niki POLYKRETI ◽  
Anna KARKANI ◽  
Eirini KARDARA ◽  
Stamatina SEFERLI ◽  
...  
Keyword(s):  
Drainage Basin ◽  
Flood Hazard ◽  
Field Measurements ◽  
Infiltration Rate ◽  
Flash Floods ◽  
Annual Rainfall ◽  
The Relationship ◽  
The City ◽  
Geological Formations

Flash floods are one of the most significant natural hazards in the Mediterranean, affecting most basins in the region. Flash floods usually occur in ephemeral streams after particularly heavy rainfall. Although the average annual rainfall in the Cycladic islands (Greece) does not exceed 400 mm, flash floods are frequent, since most of that rainfall is often concentrated in few but very intense events. The case study is the drainage basin of Paratrechos or Peritsi stream in Naxos Island. This particular basin was selected due to the recorded flood events, the stream's proximity to the city that intensifies the flood impact, the slopes' gradient abrupt changes and the diverse infiltration rate of the geological formations. Furthermore, some parts of the basin are intact by human activities, while others are severely affected. This study investigates the relationship between rain and runoff through Unitary Hydrographs, in order to estimate and evaluate the flood potential of the aforementioned hydrologic basin and to determine the causes of the hazard and vulnerability. The Clark method was implemented and its results were further evaluated by field measurements.

scholarly journals Topography Impacts Hydrology in the Sub-Humid Ethiopian Highlands

Water ◽  
2022 ◽  
Vol 14 (2) ◽  
pp. 196
Author(s):  
Demesew A. Mhiret ◽  
Minychl G. Dersseh ◽  
Christian D. Guzman ◽  
Dessalegn C. Dagnew ◽  
Wubneh B. Abebe ◽  
...  
Keyword(s):  
Water Table ◽  
Surface Runoff ◽  
Management Practices ◽  
Infiltration Rate ◽  
Watershed Hydrology ◽  
Ethiopian Highlands ◽  
Topographic Position ◽  
Tropical Highlands ◽  
Average Water ◽  
The Relationship

Understanding the relationship between topography, hydrological processes, and runoff source areas is essential in engineering design, such as predicting floods and implementing effective watershed management practices. This relationship is not well defined in the highlands with a monsoon climate and needs further study. The objective of this study is to relate topographic position and hydrological response in tropical highlands. The research was conducted in the Debre Mawi watershed in the northwest sub-humid Ethiopian highlands. In the monsoon rain phase of 2017 and 2018, groundwater depth, infiltration rate, and surface runoff were monitored at the upslope, midslope, and downslope positions. Surface runoff rates were measured in farmer fields through distributed V-notch weirs as estimates of positional runoff. Average water table depths were 30 cm deep in the downslope regions and 95 cm in the upslope position. The water table depth affected the steady-state infiltration rate in the rain phase. It was high upslope (350 mm h−1), low midslope (49 mm h−1), and zero downslope. In 2017, the average runoff coefficients were 0.29 for the upslope and midslope and 0.73 downslope. Thus, topographic position affects all aspects of the watershed hydrology in the humid highlands and is critical in determining runoff response.

Pendekatan Hidrogeomorfologi Dan Pendugaan Geolistrik Untuk Identifikasi Potensi Airtanah Di Jedong Malang

2021 ◽  
Vol 3 (2) ◽  
pp. 84-96
Author(s):  
Ferryati Masitoh ◽  
Alfi Nur Rusydi ◽  
Ilham Diki Pratama
Keyword(s):  
Infiltration Rate ◽  
Groundwater Potential ◽  
Dryland Agriculture ◽  
Soil Material ◽  
Ridge Area ◽  
Sandy Material ◽  
Potential Groundwater ◽  
Geomorphological Processes ◽  
Water Outflow ◽  
The Relationship

This study aims to identify the potential groundwater in Jedong, Malang, East Java. The hydrogeomorphological approach is a suitable approach to describe the relationship between hydrological and geomorphological processes on and below the earth's surface. The survey of geoelectricity complements the hydrogeomorphological approach. It will give a better description of the groundwater conditions below the earth's surface. Based on the research, there are 2 hydrogeomorphological units in the study area, which are: Volcanic Foot Valley Unit and Volcanic Foot Ridge Unit. The best groundwater potential is in Volcanic Foot Valley Hydrogeomorphological unit, namely Awar-awar Valley and Cokro Valley. The valleys are dominated by gully erosion and landslides. They have surface deposits up to a depth of 7 meters, and lots of outcrops of breccia, pumice, and andesite boulders. The valley’s springs discharge between 56 - 198 m3/day. The average infiltration rate in the valley is 1776 mm / hour, with sandy soil material. The best aquifer consisting of sandy material is more than 10 meters in depth, based on the geoelectrical survey. Water in the aquiclude layer, cannot be exploited because it is breccia and tuff material. The Sawah valley cannot be exploited further because the groundwater potential is very low. This can be identified by the thick water outflow seepage. In the Volcanic Foot Ridge Hydrogeomorphological unit, the groundwater potential is also very small. Hydrogeomorphically, water will flow down the slope to the valley. It will reduce the infiltration rate. In general, the ridge area is only used for settlement, while the slopes are used for dryland agriculture. The geoelectric analysis results show that the groundwater potential is at a depth of more than 45 meters. This research’s results show that the combination of the hydrogeomorphological approach and the geoelectric use will provide a better description of the potential groundwater. 

Swine Finishing Room Air Infiltration: Part 2. Infiltration as Affected by Room Characteristics

2018 ◽  
Vol 34 (4) ◽  
pp. 735-745
Author(s):  
Harishchandra T Jadhav ◽  
Steven J Hoff ◽  
Jay D Harmon ◽  
Daniel S Andersen
Keyword(s):  
Linear Regression ◽  
Power Law ◽  
Infiltration Rate ◽  
The United States ◽  
Design Criterion ◽  
Large Variability ◽  
Infiltration Rates ◽  
Air Infiltration ◽  
Ceiling Height ◽  
The Relationship

Abstract. Data collected on 17 swine finishing rooms from the Midwest region of the United States was used to study the relationship between infiltration rate and selected room characteristics. Effect of individual room characteristics on room infiltration rate were tested by simple linear regression (SLR) while multiple linear regression (MLR) was used to develop models for improved prediction. SLR results revealed that the total (It) and other (Io; non-curtain/fan locations) swine finishing room infiltration rates were inversely related to room width and directly related to room length and ceiling height. As expected, rooms with higher curtain end pocket overlap, curtain closure overlap distance, and in excellent condition had reduced curtain infiltration (Ic). To reduce fan infiltration (If), fan and pump-out cover perimeter and fan area should be minimized. Power law equations fitted for groups of rooms were found ineffective in accounting for the large variability in infiltration rates of swine finishing rooms as compared to MLR models. MLR models developed for It and Io prediction at 10, 20, and 30 Pa pressure differences were found to improve the prediction over power law models for groups of rooms. At 20 Pa, prediction differences compared with individual room measurements for It rate using the suggested MLR model, as compared to power law models for groups of rooms, were less by at least 61%; whereas, in the case of Io rate, prediction differences compared with individual room measurements were less by at least 49%. Recommendations made in this article, with respect to the relationship between a particular room characteristic and room infiltration rate, could be used as guiding principles along with other design criterion to reduce infiltration rates in remodeled and new swine finishing rooms. Keywords: Infiltration, Swine finishing rooms, Ventilation.

scholarly journals Root mass may affect soil water infiltration more strongly than the incorporated residue

F1000Research ◽  
2019 ◽  
Vol 7 ◽  
pp. 1523
Author(s):  
Masato Oda ◽  
Burhanuddin Rasyid ◽  
Hide Omae
Keyword(s):  
Soil Erosion ◽  
Soil Water ◽  
Crop Residue ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Root Mass ◽  
Soil Water Infiltration ◽  
Residue Incorporation ◽  
Crop Residue Incorporation ◽  
The Relationship

Crop residue incorporation increases stable soil pores and soil water infiltration, consequently, reduces surface water runoff and soil erosion. However, few studies have examined the relationship between crop residue incorporation and water infiltration. A previous study showed that water infiltration increases depending on the quantity of applied wheat straw. In this study, we examined whether the relationship is applicable to different crop residues in a crop rotation. We grew corn, rose grass, and okra in crop rotation under greenhouses and measured the water infiltration rate at the time of ridge making. A strong correlation was found between the quantity of applied residue and the soil water infiltration rate ( r = 0.953), although there were outliers in the case of no prior crop. By contrast, aboveground biomass of the prior crop showed a stronger correlation with water infiltration rate ( r = 0.965), without outliers. Previous studies have revealed the exponential relation between plant root mass and soil erosion. Our data also show a positive relationship between resistance to erosion and root mass when assuming that aboveground biomass is proportional to the underground biomass. The result also showed that the effect of the prior crop root mass disappears within the next crop period. This suggests that maintaining a large root mass is crucial for reducing soil erosion.

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