A simple, low-cost method was developed to collect, transport and

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A SIMPLE, LOW-COST METHOD TO COLLECT UNDISTURBED CORES OF ACID SULFATE SOIL PROFILES FOR THE STUDY OF WATER AND SOLUTE MOVEMENT DURING RECLAMATION AND USE FOR WETLAND RICE Le Ngoc Sen The International Rice Research Institute Los Baños, Philippines 1 Summary A simple, low-cost method was developed to collect, transport and instrument undisturbed soil profile cores. This method was used to test different combinations of measures to reclaim acid sulfate soils for wetland rice. The cores are large enough to accommodate several rice hills until maturity. Oil drums of 60 cm inside diameter and 90 cm length were used as lysimeter cylinders. Their surfaces were coated with epoxy paint to prevent contamination of the soil material. These cylinders were inserted into the undisturbed soil by pressure aided by excavation and trimming around the cutting edge. Soil profiles to 0.85 cm depth were thus obtained. The filled cylinders were brought to the experiment station after sealing their bottoms. Perforated PVC drainage pipes, capacitive soil moisture probes and soil moisture sampling filters were installed at different depths to drain water from the profiles, to measure the changes in soil moisture content during the oxidation process and to monitor the composition of soil solutions during reclamation and crop growth. The present paper only describes the design of the lysimeter drums and the methods of collection and instrumentation. 2 Introduction Research on acid sulfate soils has largely been of two main types: 38 1

fundamental laboratory experiments on individual, disturbed soil samples the results from which are not directly transferable to field conditions and reclamation trials in the field that generally do not allow for sufficient measurements to determine the rate and extent to which the different processes influence soil conditions and crop growth. Undisturbed soil cores of large size are desirable for the study of the dynamics of soil physical and chemical changes in a closely controlled system that is similar to the field situation. Techniques to obtain undisturbed soil cores have been reported by different workers, (Bannink et al. 1977, Black and Raines 1978, Craswell 1979, Mielke 1973 and Watson and Lees 1975). These methods are used to collect either small samples or large samples mostly for physical studies, but are not suited for the study of water and solute movement without contamination in a system with several growing plants. To answer the purpose a lysimeter drum was developed that met the dimensional requirements and limitations of the specific studies and prevailing field situations. 3 The lysimeter drum 3.1 Design requirements and construction The design specifications for a lysimeter containing an undisturbed soil profile should satisfy the following requirements: a) The lysimeter drum should be of a size and weight that allows collection of a representative soil profile core in swampy areas. b) Samples should be large enough to accommodate several rice hills until maturity to minimize boundary effects and to average out the effects of macrostructural heterogeneities in the rhizosphere on the growth of the rice. c) The gross weight of the soil profile core should be small enough to facilitate transport to the experiment station. d) The materials used should be resistant to corrosion and should not contaminate the soil profile core. Available oil drums were used to construct the lysimeters. Each has an inside diameter of 60 cm and a length of 90 cm (Figure I ). Both ends of the drum were cut out by hammer and cold chisel. The rolled edges of the drum were retained. The reinforcement ribs around the drum wall were 382

~ filled with two-component plastic putty to straighten the inside wall. Holes were drilled in the drum in different positions along its length for later insertion of perforated PVC drainage pipes, soil-moisture sampling filters and capacitive soil moisture probes (Figure 1). These are used to drain the water from the profiles to monitor solute concentrations and to measure changes in soil moisture content with time along the soil profile. The holes were sealed temporarily by epoxy-painted pieces of sheet metal glued on with two-component epoxy blue. Galvanized iron covers were fabricated for bolting to the bottoms of the drums after collecting the profile cores (Figure 1). The drums and covers were painted with epoxy paint to prevent rust and contamination of the soil. I 60cm Holes fa la:er intersection soil- water sampler Perforated PVC pipes Nut Figure I. Diagram of a lysimeter 3.2 Collection of soil profile cores The procedure used in obtaining the samples was to press the drum into the soil in depth increments of 5 to IO cm by means of a wooden bar placed on top and six to ten persons stepping on it (Figure 2A). Before each incremental insertion of the drum the soil was trimmed from around the drum to a depth of 5 to IO cm below the bottom of the cutting edge, so that only a small amount of soil had to be pared away by the cutting edge when the drum was pressed into the soil. The process was continued to the desired depth. The soil below the cutting edge was then cut in a cone shape to prevent fracture of the core while it was 383

dragged out of the profile pit (Figure 2B). One side of the profile pit was cut to a 45 slope. The filled drum was tied with rope, turned 45 degrees (Figure 2C), laid into a wooden pallet and dragged up to the ground surface along the sloping side of the pit. The excess soil material at the bottom was trimmed level with the cutting edge. A galvanized iron cover was then bolted on to close the bottom of the drum (Figure 2D). Figure 2. Scheme of field operating procedure to take undisturbed soil cores If more than one core was to be collected the drums were placed in a row to save digging effort. Experience has shown that ten men can complete collection of 5 cores per day. 3.3 Installation and instrumentation of lysimeters The joint between bottom cover and drum was sealed with two-component plastic putty. A perforated PVC drainage pipe of 2 cm outside diameter wrapped with nylon mesh (mosquito screen) was installed from the side of the drum at a depth depending on the treatment. Soil moisture sampling filters, consisting of a Whatman filter tube wrapped with micropore material, were connected with glass tubes and supported by a plastic pipe with the same outside diameter as the available filters (Figure 3). These filter assemblies were installed horizontally at different depths along the profile. 384

Rutber Stopper Whatmon Filfer Tube.Plastic cover Figure 3. Soil-water sampler components Before installing the filter assemblies, a narrow tube was bored out with a soil auger made of plastic to prevent contamination. After installing the assemblies, the joints of the plastic pipes with the lysimeter drum were sealed with two-component epoxy glue. The capacitive soil moisture probes will be installed in the same way from the opposite site of the drums. A fiberglass blanket was wrapped around the lysimeter drums to minimize horizontal heat transfer resulting from direct sunshine on one side of the drums (Figure 4). A vacuum pump is used to draw soil solution from the sampling filters into collecting tubes (Figure 5). 385

Figure 4. Lysimeter cylinders wrapped with fiber-glass blankets, first rice crop near maturity Figure 5. Lysimeter cylinder with vacuum pump and collecting tubes attached to the soil moisture sampling filters 386

4 Performance and results Experiments with lysimeter drums collected and instrumented by this method can provide information on several aspects important for the reclamation of acid sulfate soils, including leaching requirements, oxidation-reduction processes in the soil profile, and acidity build-up during the oxidation period. The cost of this lysimeter is about US $ 60: one third of the cost of fiberglass or PVC pipes of the same size. Forty-eight undisturbed soil profile cores, 80 to 85 cm long, were obtained from different places in the Philippines. These are being used to study the effects of different combinations of water management and agronomic reclamation measures on the physical and chemical changes in two acid sulfate soils: a Sulfaquept and a Sulfaquent from the Philippines. Results will be reported in a later paper. Initial observations indicate that water movement slows down after leaching the cores for one month, probably due to clay sealing off the moisture sampling filters and drainage pipes. Acknowledgements The author wishes to acknowledge the help and encouragement from Dr. S.I. Bhuiyan, Head of Irrigation Water Management Department, and Dr. R. Brinkman, visiting soil scientist, of the International Rice Research Institute. 387

References Bannink, D.W., P. Poelstra and M.J. Frisse1 1977. An installation for transport and accumulation studies on undisturbed soil columns under controlled conditions. Netherlands J. Agric. Sci. 25: 126-135. Black, J.H. and M.G. Raines 1978. Soil sampler with retrievable liner. J. Soil Science 29: 271-276. Craswell, E.T. and E.G. Castillo 1979. A convenient device for taking large undisturbed samples of paddy soil. International Rice Res. Newsl. 4(4): 22. Mielke, L.N. 1973. Encasing undisturbed soil cores in plastic. Soil Science Soc. Amer. Proc. 37: 325-326. Watson, K.K. and S.J. Lees 1975. A procedure for the sampling and testing of large soil cores. Soil Science Soc. Amer. Proc. 29: 589-590. 388