Tuesday, January 3, 2017
Cape Bojeador, Paoay Sand Dunes, Kapurpurawan White Rocks, Bangui Windmills, Pagudpud Resorts, and Cagayan River: Just a few of North Luzon’s wonders worth visiting
A tour around the northern tip of Luzon is really an amazing experience. For those interested in our natural environment, it is a must. This short report describes briefly some of the wonderful places that one can visit starting from Vigan City in the west (1) to Cagayan Valley in the east (10).
Vigan is an old city in Ilocos Sur with well-preserved Spanish colonial and Asian architecture. This UNESCO World Heritage site reminds me of some small towns in southern Spain. It is without question the most beautiful old city in the Philippines.
The Paoay Sand Dunes
The sand dunes area appears to be a raised sea bed. First evidence of this is the fact that it is directly adjacent to the sea. Second reason is the presence of shells of marine organisms in many parts of the area. Third, a road cut exposure east of the sand dunes reveals thick sandstones (formed under the sea) which could be the source, through weathering, of the sand particles. The subduction of the Sunda Plate underneath the Philippine Mobile Belt produced the Manila Trench in the South China Sea and has resulted in the uplift of northwest Luzon. Decades of soil mismanagement and the resulting soil erosion have without doubt contributed to the spread of the sand dunes.
This is the headland at the northwestern tip of Luzon in Burgos, Ilocos Norte. The raised marine terrace is flanked to the east by steep-sided volcanic and greywacke hills and to the west by the turbulent South China Sea. Perched on top of the hill at about 90m asl is the famous Cape Bojeador Lighthouse constructed in 1892 during the Spanish Colonial period.
Kapurpurawan White Rock Formation
The famous white rock formation in Kapurpurawan, Burgos, is actually a raised reef limestone that has been carved by the waves through time. The raised limestone is associated with the uplifting of northwest Luzon as a result of the subduction of the Sunda Plate underneath the Philippine Mobile Belt as has been mentioned above.
Standing 70 m tall on the black sand beach of Bangui, Ilocos Norte, are 20 giant wind turbines (giant fans) facing the South China Sea in the direction of Taiwan. The area is so windy making it ideal for such a modern energy harvesting facility.
A large resort and convention center called Hanna’s Beach Resort is found near the northernmost tip of Luzon and hidden from the highway by the mountain range in Balaoi, Pagudpud, Ilocos Norte. The bay, which has fine white sand, is unique in its location and local geography. A chat with the locals would reveal controversial stories about the real owner of the resort.
One of the many major infrastructure projects of former President Marcos is the Patapat Viaduct in Pagudpud, Ilocos Norte. The 1.3 km bridge is elevated about 30 meters above the sea and connects the Maharlika Highway from Laoag, Ilocos Norte to the Cagayan Valley Region. It is now part of the Asian Highway network (AH 26).
Anahaw or anahau (Livistona rotundifolia) is an erect palm that is widespread in northern Luzon particularly in Claveria, Cagayan. This makes the landscape in this part of Luzon different to the monotonous coconut plantations in the Visayas.
The Cagayan River
The Cagayan River (the Rio Grande de Cagayan) is considered as the second largest river in the Philippines next to the Rio Grande de Mindanao. The mighty river in the Cagayan Valley region traverses the provinces of Nueva Vizcaya, Quirino, Isabela and Cagayan and has a drainage area of about 27,300 square kilometers. The picture below shows the river from the Magapit Bridge in Magapit, Cagayan.
Soil Degradation in Cagayan Valley
Deforestation followed by decades of grazing (pasture) have caused widespread soil degradation in Cagayan Valley. This is clearly observable from Tuguegarao City down to Enrile and Sta Maria, Cagayan where the traveler sees an endless view of denuded and degraded hills and mountains.
Sunday, October 23, 2016
President Rodrigo R. Duterte emphasized the conduct of soil analysis in the country during his first State of the Nation Address (SONA) on July 15, 2016. He said that “we shall also conduct a nationwide soil analysis to determine areas most suitable for rice farming to optimize production with the use of effective soil rehabilitation and fertilization.”
As an effect of this presidential pronouncement, many people including professionals from various academic fields have been wondering what soil analysis is. Several readers of this blog suggested that I write about this topic hence, this article.
Soil analysis refers to the measurement of soil physical, chemical, and biological properties. It is done, depending on the type of soil analysis, for the following purposes: 1) to evaluate the origin and formation of the soil; 2) to assess the level of contamination of the soil; 3) to characterize the soil as a habitat of soil organisms; 4) to assess the soil fertility status; and 5) to evaluate the soil’s suitability for certain crops. Soil analysis is generally synonymous with soil testing. The major steps of soil analysis are soil sampling (and field soil examination) and laboratory analysis.
|Soil profile examination and sampling to evaluate the origin of the soil|
The first type of soil analysis is the most difficult and complex type. It is carried out by soil specialists called pedologists. It involves detailed field description of the soil using standard procedures such as the Guidelines for Soil Description (4th edition by Jahn et al., 2006) published by FAO, Rome. Soil description is done on newly dug soil pit at least 1.5m deep or fresh road cuts. Collection of soil samples for intensive laboratory analysis is done on every soil layer (soil horizon) down to the bedrock. Laboratory analyses include the physical, chemical and mineralogical properties of the soil. Geochemical analysis of rock samples is also necessary.
The second type is conducted by soil scientists interested in soil pollution or contamination. Soil samples are usually collected in areas where soil contamination is suspected. Soil sampling is done at random or at fixed interval. Only the top soil layer (0-10 or 0-20 cm) is sampled using a soil auger or similar sampling tool. Soil samples are analyzed for their contents of soil pollutants (e.g. heavy metals) and are compared with published threshold values to know if the sample is contaminated or not.
|Soil sampling to assess the contamination of Taft River in E. Samar|
The third type of soil analysis is conducted to know if the soil is favorable for certain soil organisms of interest (e.g. earthworms). This is popular among soil ecologists. Soil samples are collected usually from the top soil layer and then they are analysed for soil physical and chemical properties. Correlation analysis is then done between the population of the soil organism and the different soil properties to know which among the soil properties influences the population of the organisms.
The fourth type is the most well-known and commonly done type of soil analysis to support crop production. The main purpose is to know if the soil is fertile or not. Specifically, it is performed to assess, using high-tech laboratory equipment, if the soil contains sufficient amounts of the essential nutrients required by plants (crops) to grow well and produce good yield (grain, tubers). The essential nutrients that the pant takes up from the soil include: nitrogen (N), phosphorus (P), potassium (K), calcium (Ca), magnesium (Mg), sulphur (S), iron (Fe), manganese (Mn), copper (Cu), zinc (Zn), molybdenum (Mo), boron (B), chlorine (Cl) and nickel (Ni). Since N, P and K are required by the plant in largest amounts, these three are usually the nutrients that are of limited supply in the soil. So farmers need to know how much of these nutrients must be applied to the soil through fertilizers. The final result of this type of soil analysis is a fertilizer recommendation.
|Soil sampling for fertility evaluation|
The fifth and last type of soil analysis is carried out to assess if a certain soil is suitable for crops such as rice, corn, vegetables, fruit trees, and others. This involves field soil examination to know the soil’s texture, structure, drainage, slope and depth using the methods of the first type of soil analysis. The soil samples are analysed for soil chemical properties such as soil pH, organic matter content, nutrient holding capacity as well as the amounts of the major nutrients (similar to the third type of soil analysis). The soil properties are then matched with the ecological requirement of the crop. The final result is a suitability map or table showing the suitable crops for each soil. It also indicates the soil constraints (or problems) if a crop is grown in a soil that is not suitable for that particular crop.
From the president’s pronouncement, it looks like that he meant the fifth type of soil analysis. Due to the tremendous amount of field and laboratory works, it cannot be done by the Bureau of Soil and Water Management alone. It needs the participation of universities with strong soil science program throughout the country such as Central Luzon State University, University of the Philippines Los Banos, Visayas State University, Central Mindanao State University, and University of Southern Mindanao.
|Soil science students at VSU performing laboratory analysis of soil samples|
The laboratory step of soil analysis or soil testing is tedious, time-consuming, and costly because the chemicals and apparatus required are very expensive. Although there are some rapid soil test kits available, they are not reliable. Also, the laboratory analysis has to be done according to accepted procedures and by trained personnel. Examples of accepted procedures of laboratory analysis of soils are:
Carter M.R. and E.G. Gregorich (Eds.). 2008. Soil Sampling and Methods of Analysis (2nd ed). CRC Press, Boca Raton.
International Soil Reference and Information Center (ISRIC). 1995. Procedures for Soil Analysis (L.P. Van Reuwijk, Editor). Wageningen, the Netherlands.
Jones J. B. Jr. 2001. Laboratory Guide for Conducting Soil Tests and Plant Analysis. CRC Press, Boca Raton.
Margesin R. and F. Schinner(Eds.). 2005. Manual for Soil Analysis – Monitoring and Assessing Soil Bioremediation. Springer Verlag, Berlin.
Pansu M. and J. Gautheyrou. 2006. Handbook of Soil Analysis. Mineralogical, Organic and Inorganic Methods. Springer Verlag, Berlin.
Schlichting E., H.P. Blume and K. Stahr. 1996. Bodenkundliches Praktikum (Soil Science Practicum). Blackwell Wissenschaftsverlag, Berlin.
Sparks D.L., A.L. Page, P.A. Helmke and R.H. Loeppert (Eds.). 1996. Methods of Soil Analysis Part 3—Chemical Methods. Soil Science Society of America, Madison, Wisconsin.
Westerman R.L. (Ed.). 1990. Soil Testing and Plant Analysis (3rd ed). Soil Science Society of America, Madison, Wisconsin.
Thursday, September 15, 2016
Refocusing Agriculture: Excerpt from my Convocation Speech at the 45th Founding Anniversary of Visayas State University (VSU)-Alangalang Campus, Leyte, Philippines on 09 Sept 2016.
By V.B. Asio
Your theme “Agrivolution: refocusing farming for food and nutrition security” is very timely and very relevant.
When I was an agriculture student in ViSCA in 1980, the agriculture battle cry was: we need to increase crop yield by increasing the yield per unit area and by cultivating new lands because of rapidly increasing population. Population of the country at the time was only 48 million. The hot research topic was farming system, which slowly became cropping system, then sustainable agriculture or ecological farming, and now organic agriculture. If you examine these farming strategies, they are closely related. But the last, which is organic agriculture, has become very narrow in scope and very impractical in many aspects.
|Highly productive alluvial lands in Baybay, Leyte, are threatened by conversion into residential areas|
But where are we now?
Now more than 30 years have passed, with a staggering country’s population of more than 100 million, we still have the same battle cry: to increase food production by increasing yield per unit area and by opening new lands. This time though, there are a lot more complications. The problem of increasing food production has become more urgent, and very problematic. Let me cite some reasons:
1. The gap between population increase and food production has greatly widened. Our population has more than doubled but crop yield has not doubled despite the availability of new high yielding varieties, fertilizers and pesticides. For example, average rice yield in 1980 was 2.3 tons/ha. Now it is only 3.8 tons/ha. What is aggravating the problem is that production cost has greatly increased, and the area of our agricultural lands have decreased.
Many of the new high yielding varieties which showed great potential in the experimental stations, have failed to show their yield potential in the actual world-- in farmers’ fields . According to Dr. Francisco of Philrice in an undated paper, the yield gap ranges from 2 t/ha in the wet season, to 3.9t/ha in the dry season. This also partly explains why we cannot find our new high yielding varieties (say, of sweetpotato) in farmers’ farms in Leyte and Samar.
2. There is increasing soil degradation due to destructive farming practices, resulting in the decline in soil fertility. This is coupled by increasing incidence of pests and diseases. The latter triggers the farmers to over apply pesticides. In our on-going ACIAR-funded soil research, vegetable farmers in the Visayas and some parts of Mindanao just apply any amount of fertilizers without scientific or logical basis. Worse, they over-apply a cocktail of pesticides, 2-3 times a week, endangering the health of the consumers.
3. As if to make matter more difficult for the next generation, the widespread soil degradation is accompanied by the shrinking of our prime agricultural lands because of urbanization. Urbanization is eating fast our rice lands. In many parts of the country, you would see former productive rice lands have become subdivisions, factory sites and shopping malls.
4. Climate change has entered the picture. It has changed rainfall pattern, temperature fluctuations, and occurrence of typhoons, floods, and drought. Crops are now subject extreme weather conditions. In short, we are in a more challenging and exciting agriculture.
5. As a result of the over-application of farm inputs, there is also a degradation of the environment. Soil, water and air pollution are very serious in many places.
6. This has led to the rise of the organic agriculture movement. The Philippine government has enacted the Organic Agriculture Act of 2010. But we know that organic agriculture cannot produce the amount of food required to feed the fast rising population of the country. Organic agriculture cannot feed our more than 100 million population.
So, we are now facing a dilemma: protect the environment even if the food production is low, or continue the environmentally damaging practices but with a higher food production. This is like the choice between the ocean and the deep blue sea.
7. The Genetically Modified Organisms (GMO) technology hold great promise for some crops, but are we sure that they are safe? The debate is raging in the international scientific community. Time will tell if GMO crops are really safe to our health and to the environment.
8. Despite the more than 40 years of designing of agricultural implements, most of our farmers are still practicing manual labor due to a lot of reasons. Have we really looked into why majority of our farmers are not using modern farm implements until now?
9. What threatens further our agriculture is the decreasing interest in farming among our young generation. It seems everybody wants a happy and easy life. Interest in agricultural science has continued to decline as reflected by the general decline in enrollment in universities and colleges around the country (fortunately, our enrolment in agricultural sciences at the main campus has continued to increase in the last five years).
10. The mainstream media are partly to blame. Just observe what kind of TV programs are created and promoted. To cite an example, beauty contests are very popular because of the intense media campaign. No wonder many young girls dream to be a beauty queen instead of becoming scientists. The media have failed to create awareness among the youth about the importance of agriculture or about science. And of course, our government institutions too. Much of the blame should go to them.
What should we do? How can we refocus farming or agriculture?
The problem is so serious and so complex. It needs the active participation of all sectors involved. As an academician, I will just focus on the things that we can do in the academe.
1. There is a need for retooling of those involved in teaching students agriculture. Agricultural science now is different in many aspects from that 30 years ago.
2. We need to revise and improve our curricula and the courses we are offering.
3. We need to change our strategy in promoting agriculture. If we still project agriculture using the image of a farmer with the plow and the carabao, we will not gain bright young students to agricultural science.
4. There is a need for more involvement of our students in OJT in successful and progressive farms.
5. We need more reliable data on the effects of fertilizers on crop yield. In the last decade, everywhere, there has been a sprouting of all kinds of organic fertilizers whose efficacy have not been scientifically verified. Proponents just cite anecdotal evidence to promote their products. This has led to the erosion in people's confidence in organic fertilizers.
6. We need to change our strategy in extension. We need to educate more our farmers. How? It is for all of us to think about.
Before I end my talk let me quote Masanobu Fukuoka, a Japanese farmer and philosopher. He said that:
“The ultimate goal of farming is not the growing of crops, but the cultivation and perfection of human beings.”
Thank you for your kind attention. Happy 45th Anniversary to VSU-Alangalang!
Thursday, September 1, 2016
Tropical regions occur between the Tropic of Cancer and the Tropic of Capricorn. The tropics include approximately 40% of the land surface and is the largest ecozone of the earth. According to Köppen (1931), the tropics are characterized by an annual mean air temperature above 18°C throughout the whole year. The largest climatic variation is introduced by the variability of precipitation, reaching from nearly 0 mm in the Saharan and Atacama Desert to 11,700 mm on Mt. Waialeala in Hawaii (Eswaran et al., 1992).
|An Afisol (Luvisol) soil derived from mudstone in Eastern Samar, Philippines|
According to Uehara and Gillman (1981), "tropical soils" is a common name used to identify any soil that occurs in the tropics. They noted that like most common names, the term lacks precision, but it is more readily understood by a larger audience than are the scientific names. In contrast, Sanchez (1976) argued against the use of the term "tropical soils" since it does not accurately reflect the soils in the tropics.
|Selected properties of the major tropical soils (Jahn and Asio, 2006)|
The name tropical soils is now globally accepted but these soils have remained poorly understood until now. The following are some important aspects about tropical soils (Jahn and Asio , 2006):
- The tropics, the world’s largest ecological zone, have very high potential for plant growth but with soil limitations in vast areas.
- About one-third of the soils of the world are tropical soils. The most widespread are Ferralsols, Acrisols, Luvisols, Cambisols and Arenosols.
- The large proportion of Cambisols (Inceptisols) and Luvisols (Alfisols) in Southeast Asia reflects clearly the younger age of land surfaces and therefore the short duration of weathering processes.
- Some soils occur almost exclusively within the tropics. About 90% of the Ferralsols (Oxisols), 80% of the Nitisols (Oxisols/Ultisols), and 60% of the Acrisols (Ultisols) are situated in tropical regions.
- The major soil limitations or soil constraints are low cation exchange capacity, low base saturation (low pH, high Al-saturation) and high P retention. They are most widespread in South America, Africa and Southeast Asia (in decreasing order based on area).
- Physical constraints like high groundwater table, air deficiency and low soil depth are of lesser significance but govern special requirements for soil management in specific landscapes.
- Due to severe chemical limitations, proper management of nutrients is the main challenge for effective land use systems in the tropics.
- Internal and external fluxes of nutrients are different among soil types and different among tropical landscapes. These have to be considered in ecological land use systems.
- To conserve the stock of organic matter in tropical soils (and to increase it in degraded soils), biomass productivity will be a key point for ecological land use systems.
- To enable policy-makers as well as land users to establish sustainable and ecological land use systems in the tropics, more precise soil maps and soil information are needed.
Eswaran H., J. Kimble, T. Cook & F.H. Beinroth. 1992. Soil diversity in the tropics: Implications for agricultural development. In: Myths and Science of Soils in the Tropics. SSSA Special Publ. No. 29.
Jahn R. and V.B. Asio. 2006. Climate, geology and soils of the tropics with special reference to Southeast Asia and Leyte (Philippines). In: Proc. 11th International Seminar-Workshop on Tropical Ecology, 21-25 Aug 2006, VSU, Baybay City, Leyte, pp: 23-42.
Köppen W. 1931. Grundriss der Klimakunde. W. de Gruyter & Co., Berlin
Sanchez, P.A. 1976. Properties and Management of Soils in the Tropics. Wiley, New York
Uehara G. and G. Gillman. 1981. The Mineralogy, Chemistry, and Physics of Tropical Soils with Variable Charge Clays. Westview Press, Boulder Colorado.
Tuesday, August 30, 2016
Dr. Ian A. Navarrete was recognized as one of the Outstanding Young Scientists for 2016 by the National Academy of Science and Technology (NAST), the premier and most prestigious recognition and advisory body on science and technology in the Philippines. He was awarded for his outstanding achievements in Soil Science as reflected by his papers in international journals as well as by the prestigious research awards he has won.
|Dr. Navarrete as one of the Outstanding Young Scientists in 2016 (photo by IA Navarrete)|
Every year, NAST selects 12 recipients of the Outstanding Young Scientist (OYS) Awards who should be young Filipino scientist (below 41 years old) and who have made significant contributions to science and technology.
|During the field sampling for his doctoral dissertation in the central highlands of Leyte|
Dr. Navarrete, who comes from Javier, Leyte, finished his BSA Soil Science and MSc in Soil Science from Visayas State University (VSU). He conducted his undergraduate and graduate theses under the supervision of V.B. Asio. For his MSc thesis on the characteristics and genesis of highly weathered soils from Samar, he spent four months performing mineralogical and elemental analyses at the Institute of Soil Science and Plant Nutrition, Martin Luther University, Germany (hosted by Prof. Reinhold Jahn) with scholarship support from the German Academic Exchange Service (DAAD). The thesis discovered the occurrence of an Oxisol in Samar.
|With members of the pedology group of VSU during the field work for his postdoctorate research|
He then pursued his doctorate degree at Obihiro University of Agriculture and Veterinary Medicine, Japan, and then went to the University of Goettingen, Germany, for his postdoctorate as an Alexander von Humboldt Research Fellow, a highly competitive and world-renowned fellowship. The field studies for his doctoral dissertation and postdoctorate research were conducted in Leyte in collaboration with the Pedology and Geo-ecology Laboratory (V.B. Asio) at VSU.
Since 2015, Dr. Navarrete is an Assistant Professor at Ateneo de Manila University.
Prof. Dr. Reinhold Jahn, retired professor of soil science and soil protection at Martin Luther University (also known as University of Halle-Wittenberg), Germany was given the highest award called Sandigan Award (Sandigan means someone you can depend upon) of the Visayas State University (VSU), Baybay, Leyte. In a ceremony on 03 August 2016 at the office of the president, University President Edgardo E. Tulin handed the plaque of recognition to Prof. Jahn in the presence of Dr. Wolfreda T. Alesna, Chairperson of the Awards Committee and several faculty, staff, and students of the Department of Soil Science of VSU.
|Prof. Reinhold Jahn receiving the Sandigan Award from Univ President Edgardo E. Tulin|
Prof. Jahn was recognized “for his invaluable contributions to the Visayas State University. Since 1995 until his retirement in 2012, Prof. Jahn initiated exchange of students between his faculty in Halle and VSU. He mentored and served as host professor to some VSU academic staff and students who conducted short- and long-term researches in his institute. He strongly supported by serving as resource person and lecturer the 13 editions of the international ecology seminar-workshops co-organized by VSU, University of Hohenheim, and the University of Halle-Wittenberg. During his many scientific visits to VSU in the last 20 years, he conducted several seminars and field works for graduate and undergraduate students of soil science and tropical ecology. Finally, the pioneering pedological-ecological researches on the volcanic soils of Leyte that he and his VSU colleagues have conducted and the international publications they published particularly the Guidelines for Soil Description published in several languages by the FAO of the United Nations and which bears the seal of VSU on its cover have brought international prestige to the university.”
|Field work at Lake Danao with participants of the international training on soil examination (2006)|
Prof. Jahn obtained his Diplom (MSc) from the Technical University of Berlin, his PhD and Habilitation degrees from the University of Hohenheim under Prof. Karl Stahr. He authored or co-authored several books and more than a hundred papers in international journals which have been cited more than 2,000 times (Source: Google Scholar). He has conducted research projects in Germany, Spain, various parts of Africa, China, Indonesia and the Philippines. He was elected chairman of various commissions in the German Society of Soil Science and the International Union of Soil Sciences.
|During a soil excursion to Southern Leyte with graduate students (2009)|
The formal awarding ceremony, which Prof. Jahn was not able to attend, was held at the VSU Gym on 10 August 2016 as one of the highlights of the 92nd Anniversary Celebrations of the university.
Saturday, March 19, 2016
The Scheffer/Schachtschabel Lehrbuch der Bodenkunde (Textbook of Soil Science), the renowned standard textbook on soil science in German-speaking countries such as Germany, Austria and Switzerland, is now available in English for the first time. The first edition of this highly cited book was published in 1937 under the title “Agrikulturchemie, Teil A: Boden” (Agricultural Chemistry, Part A: Soil).
Based on the 16th German edition which was written by a team of leading soil scientists (all renowned professors of soil science), the 2016 English edition was published by Springer Verlag, so it is available globally. I really applaud this development since I have always admired and used this book since the time I was a doctoral student in Stuttgart-Hohenheim many years ago and until now as a professor of soil science at Visayas State University. I remember I read the 10th German edition several times, from cover to cover, in preparation for my comprehensive examination under Prof. K. Stahr. In my opinion, this is among the best, if not the best, soil science textbook for undergraduate and graduate students available today. It is also an excellent reference for soil researchers. I have already bought an electronic copy of the book and I highly recommend it to all those interested in learning soil science.
You can also find an article about this book which I wrote in 2012 for the Bulletin of the International Union of Soil Sciences. At that time I was asked by the editor of the bulletin to name my top three soil science books.