scholarly journals Struktur Komunitas Mesofauna Tanah dan Kapasitas Infiltrasi Air setelah diberi Perlakuan Biostarter Pengurai Bahan Organik

2013 ◽  
Vol 15 (2) ◽  
pp. 81 ◽  
Author(s):  
Latifah Fitria Andriani ◽  
Rully Rahadian ◽  
Mochamad Hadi
Keyword(s):  
Community Structure ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Soil Infiltration ◽  
Infiltration Capacity ◽  
Soil Mesofauna ◽  
Randomized Design ◽  
Significant Difference ◽  
Spearman Correlation Test ◽  
Number Of Individuals

Research about the biostarter application on the biopori concept through parameter of soil mesofauna community structure and water infiltration capacity was aimed to investigate the effect of biostarter product on soil mesofauna community structure and water infiltration rate at Lubang Resapan Biopori (LRB) aged 30 days and 50 days, also the correlation between mesofauna community structure and soil infiltration capacity. This study uses a single factor completely randomized design, which has 5 treatments including control, EM4, Bioklin, Mig Dec, and Orgadec. The results showed that the addition of biostarter affects soil mesofauna community structure, particularly positive effect on the abundance of Oribatida and Mesostigmata. Products Orgadec was able to increase faster the abundance of mesofauna both at the age of LRB 30 days and 50 days, whereas Mig Dec and EM4 starting to show its influence on the LRB after 50 days. Infiltration rate LRB age of 30 days showed a significant difference in treatment of Orgadec only, whereas at the age of 50 days, the significant difference is indicated in the treatment EM4​​, Mig Dec and Orgadec. Based on the Spearman correlation test, the total number of individuals and number of Oribatida. Both showed significant positive correlation with the infiltration rate.   Keywords: biostarter, community structure, soil mesofauna, infiltration rate, LR

scholarly journals Effect of Various Compost Doses on the Soil Infiltration Capacity

2014 ◽  
Vol 62 (5) ◽  
pp. 849-858
Author(s):  
Barbora Badalíková ◽  
Jaroslava Bartlová
Keyword(s):  
Sandy Loam ◽  
Arable Land ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Soil Infiltration ◽  
Infiltration Capacity ◽  
Permanent Grassland ◽  
Water Holding ◽  
Grassland Site ◽  
Positive Effect

In the years 2008–2012, the infiltration capacity was monitored in the different sites, viz. on the arable land and permanent grassland. In the permanent grassland site the soil was characterised as Leptic Cambisol, loamy sand with the depth of the top layer 0.20 m while on the arable land, it was classified as Eutric Cambisol, sandy loam with the maximum depth of the topsoil humus horizon 0. 40 m. Experimental variants with different doses of incorporated compost were as follows: Variant 1 –without compost incorporation, Variant 2 – compost incorporated in the dose of 80 t.ha−1, Variant 3 – compost incorporated in the dose of 150 t.ha−1. It was found out within the study period that the application of the higher compost doses showed a positive effect on infiltration rate in both localities. In Variant 3, the highest values of the water infiltration were recorded. It can be concluded that the highest dose of compost (150 t.ha−1) improved and accelerated both the infiltration and water holding capacity of soil for a longer period. With the exception of the year 2009, increased values of water infiltration were recorded on experimental plots with arable land than with permanent grassland. It was found also that after five years have not been marked differences between variants. It follows that the regular supply of organic matter is necessary, preferably after three years.

scholarly journals The Effect of Soil Density on Infiltration Rate in The Urban Development Area of Padang

2018 ◽  
Vol 20 (1) ◽  
pp. 1-5
Author(s):  
Totoh Andayono
Keyword(s):  
Infiltration Rate ◽  
Water Infiltration ◽  
Density Parameter ◽  
Public Facility ◽  
Soil Density ◽  
City Development ◽  
Soil Infiltration ◽  
Infiltration Capacity ◽  
North East ◽  
Development Area

Majority of Padang City residents inhabitant the region along sea shore for residential, public facility and economic center together with all of supporting facilities. That region is seismic prone area, also potentially affected by tsunami hazard and flood.This circumstances pushed local authority of Padang City to develop urban residential area to the north, east and south side of this city (Koto Tangah, Kuranji, Pauh, Lubuk Kilangan and Bungus Teluk Kabung sub-district), which are used to be water infiltration area. The function`s shifting of this area cause the change of soil density. This condition potentially causethe alteration of rainfall infiltration in to the soil.This research was conducted at 15 locations in Dadok Tunggul Hitam area, Koto Tangah sub-district (9 locations in development area and 6 locations in original area condition). Double Ring Infiltrometer are used in this study to predict infiltration rate and Sandcone for measuring soil density.This study used Horton Model to analyze infiltration rate by quantify infiltration rate data(f), constant infiltration rate (fc) and initial infiltration rate (fo). Moreover, regression analysis were used to quantify infiltration rate in order to determine its effects to soil density parameter.The results show that for high density soil (valuegd = 1,00 gr/cm3 to 1,50 gr/cm3), final soil infiltration rate in average is 0,1 mm/minuteto 0,9 mm/minute. This condition can cause decreasingof rainfall`s runoff infiltration capacity. Meanwhile, for low density of soil (valuegd = 0,30 gr/cm3to 1,00 gr/cm3), the infiltration rate value relatively high with final infiltartion rate reached 0,22 mm/minute. This analysis demonstrated that soil density influence the infiltration rate, where 23,7 % of infiltration capacity in Padang City development area is influenced by soil density parameter (gd), and the rest is influenced by other parameters

scholarly journals A Compact Weighing Lysimeter to Estimate the Water Infiltration Rate in Agricultural Soils

Agronomy ◽  
2021 ◽  
Vol 11 (1) ◽  
pp. 180
Author(s):  
Laura Ávila-Dávila ◽  
Manuel Soler-Méndez ◽  
Carlos Francisco Bautista-Capetillo ◽  
Julián González-Trinidad ◽  
Hugo Enrique Júnez-Ferreira ◽  
...  
Keyword(s):  
Agricultural Soils ◽  
Field Capacity ◽  
Mass Conservation ◽  
Infiltration Rate ◽  
Vertical Movement ◽  
Water Infiltration ◽  
Infiltration Capacity ◽  
Silty Loam ◽  
Rain Events ◽  
Weighing Lysimeter

Infiltration estimation is made by tests such as concentric cylinders, which are prone to errors, such as the lateral movement under the ring. Several possibilities have been developed over the last decades to compensate these errors, which are based on physical, electronic, and mathematical principles. In this research, two approaches are proposed to measure the water infiltration rate in a silty loam soil by means of the mass values of a lysimeter weighing under rainfall conditions and different moisture contents. Based on the fact that with the lysimeter it is possible to determine acting soil flows very precisely, then with the help of mass conservation and assuming a downward vertical movement, 12 rain events were analyzed. In addition, it was possible to monitor the behavior of soil moisture and to establish the content at field capacity from the values of the weighing lysimeter, from which both approach are based. The infiltration rate of these events showed a variable rate at the beginning of the rainfall until reaching a maximum, to descend to a stable or basic rate. This basic infiltration rate was 1.49 ± 0.36 mm/h, and this is because soils with fine textures have reported low infiltration capacity. Four empirical or semi-empirical models of infiltration were calibrated with the values obtained with our approaches, showing a better fit with the Horton’s model.

Infiltration Characteristics of Soil Moisture in Liangping County

2014 ◽  
Vol 641-642 ◽  
pp. 183-186
Author(s):  
Shu Yan ◽  
Juan Gao ◽  
Zhong Yuan Zhang ◽  
Feng Lin Zuo ◽  
Wei Hua Zhang
Keyword(s):  
Soil Moisture ◽  
Soil Water ◽  
Infiltration Rate ◽  
Water Shortage ◽  
Water Infiltration ◽  
Soil Infiltration ◽  
Infiltration Model ◽  
Double Ring ◽  
Soil Water Infiltration ◽  
Relationship Of

In order to relieve water shortage, many countries develop water-saving industries and increase water use rate of irrigation. The research on soil water infiltration has important effect on infiltration and runoff, as well as for irrigation. The study carried out in Liangping district of Chongqing by using double ring infiltration method and exploring the reasonable infiltration model in the study area. The relationship of initial soil moisture and irrigation coefficient was studied as well. The results showed that: the Kostiakov empirical formula could simulate the process of soil water infiltration properly. The soil infiltration rate of Liangping is 0.0320cm/min in the selected location.

Storage-Infiltration Effect of Rainfall for Sunken Greenbelt in Urban Road

2013 ◽  
Vol 838-841 ◽  
pp. 1216-1220 ◽  
Author(s):  
Hu Zhu Zhang ◽  
Hui Min Li ◽  
Gui Fei Wei
Keyword(s):  
Influence Factors ◽  
Infiltration Rate ◽  
Recurrence Interval ◽  
Time Interval ◽  
Rainfall Runoff ◽  
Soil Infiltration ◽  
Infiltration Capacity ◽  
Urban Road ◽  
Design Program ◽  
Changchun City

In order to study the storage-infiltration effect of rainfall for sunken greenbelt in urban road, its storage-infiltration capacity of rainfall runoff was analyzed based on the rainfall balance equation of urban road in the time interval, and then the computational formulae of storage-infiltration rate was derived. Influence factors on storage-infiltration rate, such as design recurrence interval of rainfall, soil infiltration coefficient, greenbelt rate, and depth of sunken greenbelt, etc. were computed and analyzed by using the derived computational formulae with the rainfall intensity of Changchun city. Results show that: on the same condition, storage-infiltration rate of rainfall for sunken greenbelt in urban road increases linearly with the increase of soil infiltration coefficient, greenbelt rate, and depth of sunken greenbelt, and decreases with the increase of design recurrence interval of rainfall. Sunken greenbelt with depth of 0.05 ~ 0.25m can storage-infiltrate all of the rainfall that falls on the urban road when the greenbelt rate of urban road ranges from 20% to 40%. Eco-design program of sunken greenbelt in urban road is reasonable and feasible, and its storage-infiltration effect of rainfall is remarkable.

scholarly journals INFLUÊNCIA DA APLICAÇÃO DE VINHAÇA NA CAPACIDADE DE INFILTRAÇÃO DE UM SOLO DE TEXTURA FRANCO ARENOSA

Irriga ◽  
2010 ◽  
Vol 15 (4) ◽  
pp. 344-352 ◽  
Author(s):  
Alexandre Barcellos Dalri ◽  
Glauco Eduardo Pereira Cortez ◽  
Luis Guilherme Senarese Riul ◽  
Jairo Augusto Campos Araújo ◽  
Raimundo Leite Cruz
Keyword(s):  
Soil Erosion ◽  
Sandy Loam ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Infiltration Capacity ◽  
Rate Estimate ◽  
Erosion Risk ◽  
Soil Water Infiltration ◽  
Loam Soil ◽  
Horton Model

Este trabalho teve como objetivo estudar o efeito da aplicação de diferentes lâminas de vinhaça na infiltração de água no solo e verificar a adequação dos modelos de Horton e Kostiakov-Lewis na estimativa da taxa de infiltração. Os tratamentos corresponderam à aplicação de cinco doses de vinhaça (0, 200, 250, 300 e 350 m3.ha-1). A aplicação de vinhaça propiciou uma redução da taxa de infiltração básica do respectivo solo em estudo, causando efeito negativo para essa característica, pois, eleva o risco de erosão do solo e majora a possibilidade do escoamento superficial. O modelo de Horton propiciou o melhor ajuste sobre os dados observados, e o modelo de Kostiakov-Lewis superestimou os valores da taxa de infiltração.   UNITERMOS: vinhaça, infiltração, solo.     DALRI, A.B.; CORTEZ, G.E.P.; RIUL, L.G.S.; ARAÚJO, J.A.C.; CRUZ, R.L. VINASSE APPLICATION INFLUENCE ON INFILTRATION CAPACITY OF SANDY LOAM SOIL     2 ABSTRACT   The objective of this study was to analyze effects in different depth in soil water infiltration and to verify the Horton and Kostiakov-Lewis models adequacy in infiltration rate estimate. The treatments were five doses of vinasse (0, 200, 250, 300 and 350 m³.ha¹). The vinasse application reduced the soil erosion risk increasing the possibility of runoff. The Horton model had the best adjustment on the observed data, and the Kostiakov-Lewis model overestimated the infiltration rate values.   KEYWORDS: vinasse, infiltration, soil.

Effects of Hillslope Trenching on Surface Water Infiltration in Subalpine Forested Catchments

Hydrology ◽  
2021 ◽  
Vol 8 (4) ◽  
pp. 147
Author(s):  
Matthew C. LaFevor ◽  
Carlos E. Ramos-Scharrón
Keyword(s):  
Surface Water ◽  
Meteorological Data ◽  
Field Measurements ◽  
Water Infiltration ◽  
Human Consumption ◽  
Rainfall Runoff ◽  
Soil Infiltration ◽  
Infiltration Capacity ◽  
Forested Catchments ◽  
Total Runoff

Concerns over freshwater scarcity for agriculture, ecosystems, and human consumption are driving the construction of infiltration trenches in many mountain protected areas. This study examines the effectiveness of infiltration trenches in a subalpine forested catchment in central Mexico, where public and private organizations have been constructing trenches for ~60 years. We rely on empirical data to develop rainfall-runoff models for two scenarios: a baseline (no trenches) and a trenched scenario. Field measurements of infiltration capacities in forested and trenched soils (n = 56) and two years of meteorological data are integrated into a semi-distributed runoff model of 28 trenched sub-catchments. Sensitivity analysis and hydrographs are used to evaluate differences in total runoff and infiltration between the two scenarios. Multiple logistic regression is used to evaluate the effects of environmental and management variables on the likelihood of runoff response and trench overtopping. The findings show that soil infiltration capacity and rainfall intensity are primary drivers of runoff and trench overtopping. However, trenches provided only a 1.2% increase in total infiltration over the two-year period. This marginal benefit is discussed in relation to the potential adverse environmental impacts of trench construction. Overall, our study finds that as a means of runoff harvesting in these forested catchments, trenches provide negligible infiltration benefits. As a result, this study cautions against further construction of infiltration trenches in forested catchments without careful ex ante assessment of rainfall-runoff relationships. The results of this study have important implications for forest water management in Mexico and elsewhere, where similar earthworks are employed to enhance runoff harvesting and surface water infiltration.

Experimental Study of Influence Factors in Unsaturated Soil Infiltration Rate

2013 ◽  
Vol 477-478 ◽  
pp. 472-475
Author(s):  
Ling Cao ◽  
Xin Zhe Li
Keyword(s):  
Water Content ◽  
Unsaturated Soil ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Dry Density ◽  
Initial Water Content ◽  
Soil Infiltration ◽  
Initial Water ◽  
Cohesive Particles ◽  
Soil Infiltration Rate

Based on the unsaturated soil ponding water infiltration test in laboratory, the influences of cohesive particles content, dry density and initial water content on infiltration rate are analyzed. Soil infiltration rate decreased with the increase of cohesive particles content and dry density; with the decrease of initial water content at low dry density, and with the increase of initial water content at high dry density.

scholarly journals Temporal and spatial infiltration characteristics of soil under acacia and pine plantations in the mountainous area of Van Don, Quang Ninh, Vietnam

2019 ◽  
Vol 11 (2) ◽  
pp. 51-64
Author(s):  
Xuan Dung BUI ◽  
Thi Hoai Thu VU ◽  
Thi My Linh NGUYEN ◽  
Takashi GOMI
Keyword(s):  
Ground Cover ◽  
Infiltration Rate ◽  
Mountainous Area ◽  
Soil Infiltration ◽  
Infiltration Process ◽  
Double Ring ◽  
Pine Tree ◽  
Dye Tracer ◽  
Significant Difference ◽  
The Hill

To determine the soil infiltration characteristics of pine and acacia plantations, we used a double-ring infiltrometer in 15 different locations of up-hill, mid-hill and down-hill part in each kind of plantation from June to August, 2018. The spatial infiltration characteristics of the soil at three plots (with no tree, with acacia tree and with pine tree) was determined by dye tracer method. The factors having an impact to the infiltration process were also analyzed. The main findings include: (1) The soil infiltration rate under both pine and acacia plantation decreased over time and it was the highest in the bottom of the hill and the lowest in the middle of the hill. The infiltration rate and the total infiltrated water in one hour at the acacia plantation were higher than ones at the pine plantation. However, statistical significant difference was only found for stable infiltration rate between two plantations; (2) The area and the depth of infiltrated water were the highest at the plot without trees, smaller at the soil of acacia plot and smallest at the soil of pine plot. All spatial infiltration rates were within the findings of previous studies; (3) The result indicated that soil with high ground cover has high infiltration rate. Để xác định đặc điểm thấm nước của đất dưới rừng trồng Thông và Keo, vòng đôi đo tốc độ thấm đã được sử dụng để đo ở sườn trên, sườn giữa và sườn dưới (5 lần/ ví trí) cho mỗi loại hình rừng từ tháng 6-8/2018. Trong khi, thuốc nhuộm được sử dụng để kiểm tra đặc điểm thấm nước của đất theo không gian trên 3 ô (ô không có cây, ô trồng Keo và ô trồng Thông). Các yếu tố ảnh hưởng đến đặc điểm thấm nước cũng được phân tích. Kết quả chính thu được: (1) Tốc độ thấm ở cả hai loại rừng giảm dần theo thời gian và cao nhất ở sườn dưới,  nhỏ nhất ở sườn giữa. Cả tốc độ thấm và tổng lượng nước thấm trong một giờ của rừng keo đều cao hơn so với rừng Thông. Tuy nhiên, chỉ có tốc độ thấm ổn định là khác biệt có ý nghĩa thống kê; (2) Diện tích và độ sâu nước thấm xuống đất cao nhất ở ô không có cây, nhỏ hơn ở ô trồng Keo và nhỏ nhất ở ô trồng Thông; (3) Độ che phủ thực vật càng cao thì lượng nước thấm càng lớn.

scholarly journals The Peranan Pergerakan Air Dalam-Tanah dalam Menurunkan Aliran Permukaan

2021 ◽  
Vol 26 (2) ◽  
pp. 292-300
Author(s):  
Enni Dwi Wahjunie ◽  
Dwi Putro Tejo Baskoro ◽  
Suria Darma Tarigan
Keyword(s):  
Physical Properties ◽  
Surface Runoff ◽  
Water Movement ◽  
Initial Moisture Content ◽  
Soil Management ◽  
Infiltration Rate ◽  
Water Infiltration ◽  
Initial Water Content ◽  
Land Uses ◽  
Infiltration Capacity

The main cause of flooding and erosion that creates critical land in various regions in Indonesia is surface runoff. The surface runoff will occur if rainfall exceeds the capacity of soil water absorption (infiltration capacity). The soil management of each land use could improve the infiltration capacity. The water movement both on the surface and in the soil determines the water infiltration. This study predicts surface runoff based on the infiltration rate of various land uses and rainfall in the Ciliwung Watershed. A series of studies were performed in the upstream and middle areas of the watershed. Observations of soil properties, water movement, and rainfall were carried out in various dry land uses. The results showed that the soil's physical properties mostly determine the constant infiltration rate, which affected the water movement in the ground. The initial water content, the degree of saturation of the initial moisture content, and the soil's physical properties determine the time of constant infiltration rate. The value of constant rate infiltration and the time of its achievement define the amount of surface runoff that occurs. Keywords: hydraulic conductivity, run off, soil management, time achievement of infiltration capacity

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