HYDRODYNAMIC ANALYSIS OF COMPOST SOIL MIXTURE AND ITS IMPLICATION ON GROWTH AND POTASSIUM UPTAKE IN CORNS (Zea Mays L)

Similar documents
EXAMPLE Point A: Sandy Loam: 65% Sand _ 20% Silt _ 15% Clay. Point B: %Sand % Silt % Clay. Point C: %Sand % Silt % Clay. Point D: %Sand % Silt % Clay

Comparison of Soil Grown Cannabis Plants in a Plastic Pot, a Fabric Pot and an Octopot Grow System 1

5.1 Introduction to Soil Systems IB ESS Mrs. Page

The Effect of Potassium Humate, Chicken Feathers and Vermicompost on the Water Retention Curve

DIRT! APES Laboratory Activity

Soil CLASS. VII Soil Soil is an inseparable part of our life. Explain Humus Weathering The nature of soil: Soil Profile Horizons.

Understanding Growing Media Components

Ecological Landscaping Association's 2013 Conference & Eco-Marketplace February 27, Geoff Kuter, Ph.D. Agresource Inc.

Assessment Schedule 2015 Final Version Agricultural and Horticultural Science: Demonstrate knowledge of soil management practices (90919)

Tropical Bio-resources for Sustainable Development

0.40 Argent-Loblolly Pine. Clarksville-Shortleaf Pine 0.20 Dome-Ponderosa Pine Cohasset-Ponderosa Pine

Effect of Storage Duration in the Quality of Vermicompost

A new test procedure to measure the soil-water characteristic curves using a small-scale centrifuge

Effect of Water and Nitrogen Stresses on Correlation among Winter Wheat Organs

Soil compaction Soil Colour

Soil, Water & Plant Relationships. Lecture note for Soil and Water Management Course Prepared by Dr ND Nang

Eco new farmers. Module 2 Soil and Nutrient Cycling. Section 1 Soils and soil fertility

Availability of Calcium, Magnesium and Sulphur and Their Uptake by Amaranthus as Influenced by Composts and Fertilizers

Scheduling Irrigation for Horticultural Crops. Patrick Byers Regional Horticulture Specialist Greene County

Scheduling Irrigation for Horticultural Crops

Soil Plant Water Relationships 1

1 Determination of soil moisture content by theromogravimetric method.

1 Describe the concept of soil texture and its importance. 2 Determine the texture of a soil sample.

SOIL STRUCTURE-ORGANIC MATTER-SOIL MICRO ORGANISMS

2/19/2016. Objectives. The Basis of Life. Previous Studies. Physical Properties DYNAMICS OF SOIL INFILTRATION RATES IN VARIOUS AGRO-ECOSYSTEMS

IMPACT OF PROPAGATION MEDIA AND DIFFERENT LIGHT LEVELS ON VEGETATIVE PROPAGATION OF BEGONIAS

Soil characteristics that influence nitrogen and water management

The Study on the Plant Growth Hormones in EM A Case Study

03. SOIL WATER MOVEMENT - SATURATED AND UNSATURATED FLOW AND VAPOUR MOVEMENT - SOIL MOISTURE CONSTANTS AND THEIR IMPORTANCE IN IRRIGATION

Water Movement in Soils

1. The Nature of Soils and Soil Fertility

Why do soils differ across the landscape?

Effect of Relative Humidity on Oven Temperature of Locally Design Solar Carbinet Dryer

Bioengineering Shoreline Protection

Basic Soil Science. Fundamentals of Nutrient Management. Melissa L. Wilson

CALCULATING THE EFFECT OF ORGANIC MATTER ON SOIL WATER, NUTRIENT AND CARBON STORAGE

Loam: About 40% sand, 40% silt, 20% clay. Mixture of pore sizes to balance water retention and aeration. Considered the best soil for growing crops.

Soil Structure and the Physical Fertility of Soil

Root Temperature Effects on the Growth of Walnut and Avocado Seedlings

Soil Properties and Plant Survival

Soil Requirements of. Healthy Urban Trees

Soil is. Pieces of rock Minerals Decaying organic matter Water Air Living organisms All mixed together!

SOIL DATA: Avondale. in Allen, TX. This information was taken from NRCS web soil survey of Collin County, Texas.

CHECKLIST EFFECTS OF GROWING MEDIA CHARACTERISTICS ON WATER AND NUTRIENT MANAGEMENT

USE OF SOME SELECTED WASTES AS SUSTAINABLE AGRICULTURAL INPUTS

Understanding the Pores of a Soilless Substrate

Homework Activity Jar Test for Soil Texture

Soil Moisture and Aeration

Plant-A-Plant Water Laboratory Guide

Soil Characteristics. Soil Science 101

Influence of temperature and drying air velocity on the kinetics of convective drying in the food industry

Unit 1 Lesson 5 Soil Formation. Copyright Houghton Mifflin Harcourt Publishing Company

Lesson 3: How Deep Will It Flow?

O horizon: the O-horizon is made up of organic material. The horizon is found at the soil surface.

Specifying Soils for Plant Growth

Soil Structure, Density, and Porosity. Laboratory #4

Soil Damage From Compaction

EFFECT OF THE PACKING DENSITY ON THE MECHANICAL IMPEDANCE OF ROOT MEDIA

Retention of Water by Soil

Soils and Fertilizers. Leo Espinoza Soils Specialist

04.SOIL MOISTURE MEASUREMENT

Absorber products have the property of absorbing up to 500 times their weight in distilled water and they become gels.

Soil Chemistry. Key Terms.

Elements of the Nature and Properties of Soils Brady 3e

O M E Taha. Keywords: nanoparticles, shrinkage strain, expansive strain, nano-copper, nano-alumina ABSTRACT

ASTOUNDING as it may seem, a shovelful of soil

HORT 102: Soil Properties. Cultivated Plants: Lecture 15. [Teresa Koenig] Slide #: 1 Slide Title: Intro Information Slide

Name. There are three main types of soils called textures. They are: sand, silt, and clay. Sand has the largest particles and clay has the smallest.

Soil Organic Matter. Organic Carbon and Nitrogen. What Factors Influence the Amount of SOM? What is Soil Organic Matter? Why is SOM Important?

Managing Soils in Rangelands. Jerry Daigle

Unlock your soil s potential with K-humate

Recommended Resources: The following resources may be useful in teaching this lesson:

Unit D: Fruit and Vegetable Crop Production. Lesson 1: Planning and Preparing a Vegetable Garden Site

Problem. Can paper mill sludge be used as a fertilizer for plants and does it change the ph of the

Effect of Soil Amendment with Dry and Wet Distillers Grains on Growth of Canola and Soil Properties

IV International Symposium Agrosym /AGSY D THE INFLUENCE OF THE WAVELENGTH OF LIGHT ON SEEDLINGS LETTUCE GROWING.

Pan-African Soybean Variety Trial Protocol Training. I

CHAPTER 4 EFFECT OF TEMPERATURE AND SOIL MOISTURE CONTENT ON CUTTING ESTABLISHMENT

Soil types and soil tests

Stress-Strain and Strength Behavior of Undrained Organic Soil in Kupondol, Kathmandu

Understanding Soil Texture and Structure

Evaluation of Compost with different NPK level on pea plant under drought stress

NATURE OF SOILS OBJECTIVE:

ACHIEVEMENT LEVEL DESCRIPTORS

Soil Quality / Understanding Soil Health what are we missing?

Effect of Vacuum Cooling Operation Parameters on Cooling Time and Weight Loss of Chinese Cabbage

Increasing Production of Potato (Solanum tuberosum L.) Var. Nadia at Medium Land Through Application of Compost Goat Manure and Potassium

The Exciting World Beneath Our Feet.

Economic of Potted Gerbera with Different Growth Media under Protected Cultivation in Pune

Soils in the Field. Agronomy 105 1

Offering soil solutions for all your growing needs. and more...

Title: Lecture 16 Soil Water and Nutrients Speaker: Teresa Koenig Created by: Teresa Koenig, Kim Kidwell. online.wsu.edu

EFFECTS OF DIFFERENT GROWING MEDIA ON GROWTH AND FLOWERING OF ZINNIA ELEGANS CV. BLUE POINT

Transplant Growth and Stand Establishment of Bell Pepper (Capsicum annuum L.) Plants as Affected by Compost-Amended Substrate

Keywords: soil carbon storage, CO 2 efflux, biomass, carbon balance

Soil Stabilization by Using Fly Ash

APPLICATION DIRECTIONS SOIL BALANCE SOIL BALANCE

Soils and Land Use Test

Introduction. A soil is an earth concrete. Composition of a soil

RESPONSE OF OLIVE CULTIVARS TO ROOTING THROUGH AIR LAYERING IN DIFFERENT GROWTH MEDIA

Transcription:

Abisatya Pambayun W S et al. Special Issue, 2015, pp. 35-47 HYDRODYNAMIC ANALYSIS OF COMPOST SOIL MIXTURE AND ITS IMPLICATION ON GROWTH AND POTASSIUM UPTAKE IN CORNS (Zea Mays L) Abisatya Pambayun W S Author, Department of Bioengineering, School of Science and Technology, Bandung Institute of Technology, Bandung, Indonesia, abisatya.pambayun@gmail.com Mubiar Purwasasmita Co-author, Faculty of Industrial Technology, Bandung Institute of Technology, Bandung, Indonesia, mubiar@che.itb.ac.id Taufikurahman Co-author, School of Science and Technology, Bandung Institute of Technology, Bandung, Indonesia,taufik@sith.itb.ac.id Abstract The research has been conducted on the hydrodynamics analysis of compost soil mixture and its implications for growth and potassium uptake in corns. The study design arranged in a completely randomized method with six repetitions for soil treatment (T 0 ), a mixture of soil:compost 3:1 (T 1 ), and a mixture of soil:compost 1:1 (T 2 ) also treatment without nutrients (N 0 ), NPK with 200 kg/ha concentration (N 1 ), and NPK with 400 kg/ha concentration. (N 2 ). The research method was conducted on the porosity, capillarity and water holding test. The results showed soil:compost mix of 1:1 has a porosity value of 0.66±0.01 (11% greater than the porosity of the soil) and water holding value of 64.79±1.99 (18% greater than water holding of the soil). Corn plants grown in soil:compost mix of 1:1 has grown 35% higher than the planting of corn in soil and biomass gain of 125%. Potassium uptake in corn plants grown in compost soil mix 1:1 are 5% higher than the potassium uptake of corn plants grown in soil. This can be concluded that giving compost to the soil can improve the structure of soil and the flow of water from the soil to the plant as well as the implications for the growth and potassium uptake in plants. 35

Keywords Hydrodynamics, Soil, Compost, Corn, Growth, Uptake of Potassium 1. Introduction The hydrodynamic of the media refers to the flow characteristic of the media, especially the flow of water. Hydrodynamic characteristics can be explained as capilarity, permeability, and the ratio of water retained in the media (water holding capacity of the media). The size and shape of particles in a medium affects the flow characteristics. An example of the type of media is compost. Clumps of compost looks like soil actually has a lot of space which is shaped like capillary tubes. These capillary tubes have various size and shape that depend on the constituent materials. It will change its form from time to time continuously to form a cycle of space. It will form a system with grain of soils. Then, it will interact well with the plant root system. The pipe shape from the capillary will accommodate physical processes, chemical reactions, and biochemical processes required in physiological processes that occur in plants.. In addition to facilitate the process of physical and chemical reactions, these capillary pipes also support the survival of soil microorganisms which are useful for plants. It will accommodate the processes to be more effective and selective. This is because the space where the chemical process happens is reduced. So, the mass-energy transfer and the reaction rate will be greater. (Purwasasmita & Sutaryat, 2011). This study aims to determine the hydrodynamic characteristics which include porosity, capillary action and the ratio of water suspended in the mixture of soil and compost media. Also to determine its implications for growth and potassium uptake in corns. Nowadays trends in health food needs of consumers are increasing. Conduction of life has change in the rush of time and a lot more interesting image. As a result, some consumer groups, especially the health conscious consumer to get the nutrients while consumers around the world give priority to health. 36

2. Materials and Methods 2.1 Porosity Test Porosity test is performed using a 500 ml measuring cup filled with 135 ml of media. Then the measuring cup is filled with 200 ml of water and wait until the water certainly enter all the pores of the test medium (column) for 12 hours. Porosity of the media can be measured by the formula of porosity in the following equation. ε = (V media+v water ) V bulk (V media ) (1) With ε is the porosity, V media is the media volume on the measuring cup and V water is the volume of water that is poured into a measuring cup. V bulk is total volume of water and mediaon measuring cup after settling for 12 hours. 2.2 Capillarity Test Lu&Likos (2004) in their research states that the ratio of capillarity on media is made by looking at the high profile of water level rise over the time. Capillarity test is done using a column with a diameter of 6 cm and a height of 12 cm.the partition is given in the downside of the column to ensure the media in the column did not fall during the capillarity test. The media is poured into the column until reaching the height of 12 cm. Then, the column which contains the media is placed in a container of water.the water must be contacted withthe bottom of the media (column). Finally, the graph can be made by judging the rising water in the column every 5 minutes and observing the water level in column over the time. 2.3 Water Holding Capacity Test Water holding capacity test is done to look at the media's ability to store water which is represented as a percent of the volume of water contained in the media to the total volume of the media. Tuller and Or (2004) states that the value of retained water ratio represented as the volume of water contained in the medium divided by the volume of media used. Before the test, the weight of the media and the columns that will be used during the test are measured first. Water resistance test is begun by inserting the media into a 135 ml column with a diameter of 6 cm and a height of 12 cm. Furthermore, the column which contains the media is soaked in water 37

for ± 3 hours to ensure the mediain the column already saturated with the water. After that, the column is transferred into another container at room temperature and waited for ± 12 hours until no more water dripping through the bottom of the column. Water loss due to evapotranspiration is assumed very small so that the amount can be ignored. In the final stage, the column is measured the weight of water contained in the media using the datawhich is measured before the addition of water. 2.4 Corn Plant Growth Test Corn seeds were obtained from Balitbang Research Institution in South Sulawesi, Indonesia. The corn is a hybrid variant of Sukmaraga. Plants were grown in a green house. The medium used at the stage of sowing is soilwith the mesh of 5 (pass the filter particles of porous 4 mm) which is included in the classification of the soil silty clay containing silt at 50%, clay by 40%, and sand by 10% in the case of seeds or tray. At this stage of growth, growing medium used was a mixture of soil mesh 5: compost mesh 5 (1:1) (v: v), mixture of soil mesh 5: compost mesh 5 (3:1) (v:v), and soil mesh 5. The growing medium is placed in a polybag with the size of 20 x 12 cm (height x diameter). Each polybags filled with medium as high as 12 cm. The green house dimension is 1,5x1x1 m. Each of the green house can accommodate 54 pieces of polybag which consists of 18 pieces of polybag filled with soil: compost (1:1) (v: v), 18 pieces of polybag filled with soil: compost (3:1) (v: v), and 18 pieces of polybag filled with soil. The first stage is the sowing stage. At this stage, 98 corn seeds are sownin seed box or tray with the capacity of 98 seeds filled with soil. After 5 days, the germinated seeds are carried out to the transplanting stage. Germinated seeds are placed in polybag with the diameter of 12 cm and height of 12 cm. Each polybag is planted with onegerminated seed with the height of 5-6 cm. The third stage is the growth stage of the corn plant for 42 days. The treatment consists of three variations of media and three variations of nutrient. Variations of media consist of a mixture of soil mesh 5: compost mesh 5 (1:1) (v: v), mixture of soil mesh 5: compost mesh 5 (3:1) (v: v), and soil mesh 5. Variations of nutrient consist of variation without the addition of NPK, the addition of NPK at a concentration of 200 kg/ha, and the addition of NPK at a concentration of 400 kg/ha. So that when combined, it will create 9 varieties of plant. Each of the variation has six repetitions. 38

Ratio of Porosity MATTER: International Journal of Science and Technology The concentration of NPK fertilizer 400 kg/ha and 200 kg/ha is the number of the required area of 1 ha with a soil depth of 20 cm (Ismail, 1985). The polybags with the diameter of 12 cm and the height of 12 cm are used in this research. So, the total requirement for NPK are 0.27 gram/polybag forthe variation of 400 kg/ha (N 2 ) and 0.135 gram/polybag forthe variation of 200 kg/ha (N 1 ). Each week, the plant height is measured from the ground to the tip of the highest leaf stretched vertically. The matrix treatment of corn cultivation can be seen in Table 1. Table 1:Matrix Treatment of Cultivation Without additional nutririon (N 0 ) NPK 200 kg/ha (N 1 ) NPK 400 kg/ha (N 2 ) Soil (T0) T 0 N 0 T 0 N 1 T 0 N 2 (S:C) 3:1 (T1) T 1 N 0 T 1 N 1 T 1 N 2 (S:C) 1:1 (T2) T 2 N 0 T 2 N 1 T 2 N 2 42-day-old plants are taken for the determination of dry weight of the plant. Plant samples are dried in an oven with a temperature of 80 C for 7 days. Furthermore the samples are measured to obtain the dry weight of the plant. 3. Results and Analysis 3.1 Porosity Test 0.9 0.8 0.7 0.6 0.5 0.4 0.3 0.2 0.1 0 T0 T1 T2 Compost Media Figure 1: Porosity test on the media 39

Based on Figure 1, can be seen that the standard deviation soil porosity measurements (T 0 ) is the smallest compared to other media, this is because the shape of the soil particles that can be likened to a ball with a relatively uniform in size. Any errors in other media containing compost are due to the difficulty of ensuring the size and shape of each particle in the compost spreading evenly on one type of media, the distribution particle of compost is affecting directly to the measurement of the porosity. This result also proves that the variation of size and shape of the particles on a media will affect the amount of space contained in the media. The results of the porosity testare soil (T 0 ) 0.60 ± 0.01, compost soil mixture with a volume ratio of 3:1 (T 1 ) 0.63 ± 0.001, compost soil mixture with a volume ratio of 1:1 (T 2 ) 0.66 ± 0.01 and 0.75 ± 0.01 for the pure compost (compost) proved that compost relatively has a larger free space than the soil. Based on this result, the addition of compost can increase the space in a media with increasing levels of compost in the soil. Increasing the space on the media will have an impact on the process of respiration that occurs in a media that can facilitate the exchange of CO 2 resulted from activity at the root respiration and degradation of organic matter from the soil to the atmosphere (Yu, 2015). The pure compost has the highest value of porosity, but in its application in the field, the use of compost in full as a planting medium is less possible. Because of the other factor such as economical factor to use pure compost for the media is too costly. Therefore, based on this study, the best composition of soil and compost in terms of the porosity for growing media for the plant is a media type of soil and compost with volume ratio of 1:1 (T 2 ). 40

Water level height (cm) MATTER: International Journal of Science and Technology 3.2 Capillarity Test 14 12 10 8 6 4 2 0 0 10 20 30 40 50 60 Time (minute) T0 T1 T2 Compost Figure 2: Capillarity test on the media Based on Figure 2, it can be seen that the soil without any mixture of compost (T 0 ) has the highest water rise and the fastest compared to the other three types of media, this is because the size of the soil particles are relatively smaller and more uniform than particles of compost. The physical properties of the soil are easily to bind with water than the compost, also increasing the ability of the water to rise pass through the pores between soil particles are much larger within a shorter time. The media with a mixture of soil and compost (T1 and T2) had a high increase in the water level far enough compared with the pure compost media. It is proved that the soil particles have a significant impact in improving the increase of water level by filling the space between particles of compost. The error is large enough in the media mix of soil and compost because of the difficulty of reading the water level which indicates the distribution of the particle size of the compost is not homogeneous at any point. It reinforces the conclusion that the events capillarity occurs with rising water in the capillary tube of soil and compost is largely determined by the size of the as well as the particle size distribution in the planting medium.therefore, based on the results of this study showed that the ability of a capillary tube at compost media to lift water from the bottom is very low, so the presence of a mixture of soil and compost is a solution that is 41

Water Holding Capacity (%) MATTER: International Journal of Science and Technology right for growing media in order to maximize utilization of existing water underground to rise to the surface by utilizing capillarity events. 3.3 Water Holding Capacity Test The amount of water retained or water holding capacity as measured in this study is expressed in terms of percent (%), this figure shows the percentage of the volume of water retained in the bed of the total volume of the growing media. The amount of total water volume that can be stored in the medium is important to give the availability of water in the soil to be one of the main factors that affect plant growth. Based on research conducted by Gupta (2015), the greater the amount of water that can be retained in a planting medium will increase root length, height, number of branches, number of leaves and dry weight of a plant. Highly enough water holding capacity in medium can also minimize water consumption of crops especially grown in indoors or greenhouse, it would be very useful to improve the efficiency of water use in maintaining plant growth. Figure 3 shows the water resistance values for each type of growing media used in this study. 80.00 70.00 60.00 50.00 40.00 30.00 20.00 10.00 0.00 T0 T1 T2 Compost Media Figure 3: Water holding capacity test on media Based on Figure 3 can be seen that the largest water holding capacity in media is owned by compost. This is in accordance with the test results in which the porosity of the compost has the most free space than the other medium. The test results also explain that the water suspended 42

Height (cm) MATTER: International Journal of Science and Technology in compost media is not only found in the empty space between particles, but also because of the shape and size of the particles of compost that resembles the capillary pipes of the vascular tissue in plants so compost can store water in a relatively more longer than soil particles. It can be concluded that the compost has an important role to increase the water content in a planting medium. The importance of the influence of compost from the above results show the evidence that the soil is not enough to be a media for cultivation. Not only it has low water holding capacity, but alsothe transpiration occurs on the surface of the soil is considered quite large based on research conducted by Gupta (2015). This causes the water stored in the ground will continue to decrease over time faster than the reduction of water at the compost. Results of this study also prove that the addition of compost can increase the water holding capacity in the media. It also can retain moisture for a longer period of time. The media with ratio of soil and compost 1:1 has the best ability to holdup the water when compared to other soil mixture that is equal to 68.19 ± 1.99%. These results indicate that this type of growing media has the potential to be applied to plants that require high water content and can be applied in areas with low rainfall. 3.4 Plant Height Test 120 100 80 60 40 20 0 0 2 4 6 8 Time (Week) T0N0 T1N0 T2N0 T0N1 T1N1 T2N1 T0N2 T1N2 T2N2 Figure 4: Plant Cultivation Test Figure 4 shows the highest growth of corn plants for each treatment and nutrition media is corn plants with media soil: compost 1:1 (T 2 ) and the addition of 400 kg NPK/ha (N 2 ). It has an average height of 108 cm at week 6. It is known that all types of plants are in need for 43

Dry Biomass (gram) MATTER: International Journal of Science and Technology nutrients, both macro nutrients and micro nutrients. In the combination of compost and NPK fertilizers are eight nutrients (macro and micro) required for plant growth. Tuherkih and Sipatuhar (2008) states that if one nutrient is not available, it can lead to plant growth and development and hampered productivity. The additions of compost on media provide additional nutrients for corn plant. Because there are available nutrients in a certain amount in compost (Salundik & Simamora, 2006). The addition of compost in the media also increases the capacity of water being stored on the media so that the crop water needs can be met. 3.5 Plant Dry Biomass Dry biomass corn crop in each treatment and nutrient media can be seen in figure 4.12 corn plant samples were dried in an oven at a temperature of 80 C until dry. Corn plant dry biomass data presented in units of grams. 5.00 4.00 3.00 2.00 1.00 0.00 T0 T1 T2 Media Figure 5: Dry biomass on different cultivation media Figure 5 shows the highest dry biomass of corn plants contained on the media soil : compost 1:1 and nutrition NPK 400 kg / ha (T 2 N 2 ). The dry biomass is 4.38 ± 0.28 gram. The addition of compost in the planting medium affects the plant growth and dry biomass of the plant. The addition of compost to improve the soil structure of the chamber so that the flow of water on the soil compostmixture media is better than the flow of water on the soil media. Additionally, Tuherkih and Sipatuhar (2008) states that the addition of nutrients N, P, and K affect plant growth. 44

Potassium Absorption (ppm) MATTER: International Journal of Science and Technology 3.6 Implication of Hydrodynamic Flow on Growth and Potassium Absorption The dry biomass of corn plant is tested using AAS (Atomic Absorption Spectrophotometry) to calculate the potassium uptake. Potassium uptake in maize plants can be seen in Figure 4.13. Potassium uptake data presented in ppm (parts per million). 110 108 106 104 102 100 98 T0 T1 T2 Media Figure 6: Potassium absorption on plant Figure 6 shows, the mixture of compost soil (T 1 and T 2 ) has a value higher potassium uptake than the soil (T 0 ). In addition, increased levels of compost on the soil mix of compost also improves the uptake of potassium. This can be explained because the flow of water in the soil compost mixture to the plant is better than the flow of water in the soil to the plant. The water flow was carrying potassium which is absorbed by the plant. The structure of space in a mixture of compost and soil is facilitating water absorption to the plant. The structure of space on compost soil mixture forma branched capillary arrangement that can facilitate the flow of water to the plant. Capillary tube structure also allows the stored air to increase the surface tension of water present in the mixture of compost soil. It implicates the flow of water to the plant from the media. 4. Conclusion From the observation, it can be concluded that giving compost to the soil can improve the structure of soil and the flow of water from the soil to the plant as well as the implications for the growth and potassium uptake in plants. 45

REFERENCES Engelstad, (1997).Teknologidan Penggunaan Pupuk.UGM Press.Yogyakarta. Hafara, A., (2009). Potasium. Nutrient Edition. Retrieved from http://www.hafara.com. 29/01/2009. 2. Gupta, B., Shah, D. O., Mishra, B., Joshi, P. A., Gandhi, V. G., & Fougat, R. S., (2015). Effect of top soil wettability on water evaporation and plant growth.journal of colloid and interface science, 449, 506-513. Hakim, N., Nyakpa, M. Y., Lubis, A. M., Nugroho, S. G., Saul, M. R., Diha, M. A., & Bailey, H. H., (1986). Dasar-dasarIlmu Tanah.Universitas Lampung. Lampung, 488. Hodges, S. C., (2010). Soil fertility basics. Soil Science Extension, North Carolina State University. Ismail, P. N., (1985). Pengaruh Umur Panen Benih, Periode Simpandan Kelembaban Nisab Udaraterhadap Viabilitas Benih Jagung (Zea mays L.). JurnalInstitut Pertanian Bogor. Bogor, Jawa Barat. Lawlor, D. W., (1993). Photosynthesis.2nd Edition. Longman Group UK Limited. London. 9-23. Lingga, P. & Marsono., (2007).Petunjuk Penggunaan Pupuk. Penebar Swadaya. Jakarta. 13-36. Lu, N., & Likos, W. J., (2004).Rate of capillary rise in soil. Journal of geotechnical and Geoenvironmental engineering, 130(6), 646-650. Purwasasmita, M & Sutaryat, A., (2011). Bagian I Metode SRI-Indonesia: Rekayasa Ruang Reaktorbio Tanaman Menggunakan Bahan Setempat Kompos dan Mol. Bahan Bahasandan Pelatihan Kader DPKLTS. Salundikdan Simamora, S., (2006).Meningkatkan Kualitas Kompos. Agromedia Pustaka. Jakarta. 10. Susanto, A. B., Sardjito., Djunaedi, A. &Safuan., (2001). Studi Aplikasi Teknik Semprotdengan Penambahan Nutrien. http://nakula.rvs.uni-biefeld.de. 30/07/2008. 4. Tuherkih, E., &. Sipahutar, I. A., (2008). Pengaruhpupuk NPK majemuk (16: 16: 15) terhadap pertumbuhandanhasiljagung (Zea mays L) di tanahinceptisols. Bogor Balai Penelitian Tanah, 10-11. Tuller, M., &Or, D., (2004). Retention of water in soil and the soil water characteristic curve. Encyclopedia of soils in the environment, 4, 278-289 46

Yu, Y., Zhao, C., Zhao, Z., Yu, B., & Zhou, T., (2015).Soil respiration and the contribution of root respiration of cotton (Gossypiumhirsutum L.) in arid region. Acta Ecologica Sinica, 35(3), 17-21. 47