CHARACTERIZATION OF THE AGRICULTURAL LANDS ON THE EROSION-THREATENED SLOPES NEAR ALAQUEZ, ECUADOR
ÎÖÅÍÊÀ ÑÎÑÒÎßÍÈß ÑÅËÜÑÊÎÕÎÇßÉÑÒÂÅÍÍÛÕ ÇÅÌÅËÜ
ÍÀ ÝÐÎÇÈÎÍÍÎ ÎÏÀÑÍÛÕ ÑÊËÎÍÀÕ Â ÐÀÉÎÍÅ ÀËÀÊÅÑÀ, ÝÊÂÀÄÎÐ
©Kravchenko R.
Ph.D., Equinoctial Technological University (UTE) Universidad Tecnologica Equinoccial Quito, Ecuador, Ýòîò àäðåñ e-mail çàùèùåí îò ñïàì-áîòîâ. ×òîáû óâèäåòü åãî, ó Âàñ äîëæåí áûòü âêëþ÷åí Java-Script ©Êðàâ÷åíêî P. A, êàíä. ãåîãð. íàóê, Òåõíîëîãè÷åñêèé óíèâåðñèòåò «Ýêèíîêñèàëü», ã. Êèòî, Ýêâàäîð, roman.êã Ýòîò àäðåñ e-mail çàùèùåí îò ñïàì-áîòîâ. ×òîáû óâèäåòü åãî, ó Âàñ äîëæåí áûòü âêëþ÷åí Java-Script ©Flores Ì. J.
Quito, Ecuador, Ýòîò àäðåñ e-mail çàùèùåí îò ñïàì-áîòîâ. ×òîáû óâèäåòü åãî, ó Âàñ äîëæåí áûòü âêëþ÷åí Java-Script
©Ôëîðåñ Ì. X.
ã. Êèòî, Ýêâàäîð, Ýòîò àäðåñ e-mail çàùèùåí îò ñïàì-áîòîâ. ×òîáû óâèäåòü åãî, ó Âàñ äîëæåí áûòü âêëþ÷åí Java-Script
Abstract. The investigation is focused on the conditional characteristics of the soil on the erosion-threatened sloping lands devoted to agriculture. The studied territory is situated in the Equatorial Andes. The analyzed samples were taken from the key-sites located on the slopes with inclination angle of 10°. The comparative analysis was carried out within the borders of a key-site divided into 4 sectors with different agricultural crops: com, oats, beans and a permanent grass pasture. It is defined that the agricultural fields used for com cultivation are the most vulnerable to erosion. The organic matter content in the plow layer is decreasing up to 0,53%. The process of erosion is the leading degradation factor. Observations have shown that such erosion forms as gullies are being formed. It is recommended to reduce corn cultivation in steeply inclined areas unless erosion control measures are taken.
Àííîòàöèÿ. Èññëåäîâàíî ñîñòîÿíèå ïî÷â íà ýðîçèîííî îïàñíûõ ñêëîíàõ, èñïîëüçóåìûõ â ñåëüñêîì õîçÿéñòâå. Èçó÷åííàÿ òåððèòîðèÿ ðàñïîëîæåíà â ýêâàòîðèàëüíûõ Àíäàõ. Ïîëåâûå èññëåäîâàíèÿ çåìåëü è àíàëèçèðóåìûå îáðàçöû ïî÷â ïðèóðî÷åíû ê ÷àñòÿì ñêëîíîâ êðóòèçíîé 10 °. Ñðàâíåíèå ïðîâîäèëîñü â ïðåäåëàõ êëþ÷åâîãî ó÷àñòêà, âêëþ÷àþùåãî 4 ñåêòîðà ñ ðàçëè÷íûìè ñåëüñêîõîçÿéñòâåííûìè êóëüòóðàìè: êóêóðóçà, îâåñ, ôàñîëü, ïàñòáèùà ñ ìíîãîëåòíèìè òðàâàìè. Óñòàíîâëåíî, ÷òî ïðîöåññû äåãðàäàöèè ïî÷â íàèáîëåå èíòåíñèâíî ðàçâèâàþòñÿ íà ïîëÿõ, ãäå âîçäåëûâàåòñÿ êóêóðóçà. Íàáëþäàåòñÿ ïàäåíèå ñîäåðæàíèå îðãàíè÷åñêîãî âåùåñòâà (äî 0,53%) â ïàõîòíîì ñëîå. Îñíîâíîé ôàêòîð äåãðàäàöèè, ýòî ýðîçèîííûå ïðîöåññû. Òàêæå îòìå÷åíî ôîðìèðîâàíèå ýðîçèîííûõ ëèíåéíûõ ôîðì, òàêèõ êàê ïðîìîèíû. Ðåêîìåíäóåòñÿ îãðàíè÷åíèå âîçäåëûâàíèÿ êóêóðóçû íà êðóòî íàêëîííûõ ïîâåðõíîñòÿõ â ñëó÷àå îòñóòñòâèÿ êîìïëåêñà ïðîòèâîýðîçèîííûõ ìåðîïðèÿòèé
Keywords: erosion, soil, slop, agricultural lands.
Êëþ÷åâûå ñëîâà: ýðîçèÿ, ïî÷âà, ñêëîí, ñåëüñêîõîçÿéñòâåííûå çåìëè.
Comparative characterization of erosion-threatened areas used for agricultural crops cultivation is one of the topical issues of agriculture and the theory of erosion. The collection of soil erosion data according to various provoking factors leads to some applied recommendations. It becomes more important for the region under the investigation for the more than 40% of the population is occupied in agriculture activity.
The territory has not been thoroughly studied as far as field investigations are concerned. The developed and earlier approved mathematical models of soil erosion loss appear not to be effective for the Equatorial Andes zone [1]. Therefore, the comparative analysis of the impact that the natural conditions and agricultural crops have on the soil erosion and the degradation of slop lands carried out in the framework of field investigation process becomes particular important. A number of previous research papers have dealt with the problem of the soil degradation process in Ecuador caused by agricultural activity [2-4] and others.
The authors carried out the investigation in the province of Cotopaxi, canton Latacunga, Ecuador in 2016. The key-site is located near Alaquez, 2700-3000 meters above sea level. The location in the equtorial part of the Andes determine the main climat characteristics of the territory. The mean temperature is 12 °C, slightly varying through the months. The average annual precipitation for the region is 500-700 mm. Liquid forms of precipitation prevail. The materials for the investigation were provided by map data sources, land using data; meteorological data of The National Institute of Meteorology and Hydrology, Ecuador. ArcGIS software was applied. Field investigations were carried out. The soil sampling analysis was carried out at the laboratory of Agrocalidad, Quito.
Within the key-site (Figure 1) there are some sectors used for various agricultural crops cultivation (com, permanent grass pastures, cereals, annual plants). The analysis proved the soil to be loam.
0 1,6 3 G
III | i i i | km
Figure 1. Agricultural crops prevailing in the key-site area.
1 —- Annual plants; 2 — Pasture; 3 — Cereals; 4 — Corn.
Within each sector there were selected parts on slopes with inclination angle of 10 °. Such areas are considered to be erosion-threatened ones: the processes of linear erosion alongside with sheet wash have been observed in the area. As for the agricultural crops on the investigated slopes, the prevailing ones are oats and beans as annual plants.
The results of the organic matter content analysis in the soils of the sectors with different agricultural crops are presented on Figure 2.
(BEANS)
Figure 2. Organic matter content (%) in the slope soils of the key-site with inclination angle of 10 °.
The growing areas with oats are characterized by low rates of organic content. However, the amount of organic matter loss is the greatest in the soils of the corn fields. Cultivating corn on the slopes with inclination angle of 10 ° leads to a fast soil fertility decline. The organic matter content range of 0,53% in the plow layer reveals the soil degradation mostly caused by water erosion process. Prolong com cultivation in the steeply inclined areas of the Equatorial Andes make them lost for agriculture. The field investigation has shown the formation of gullies and rills in the territory. The conditions are favorable for active linear erosion processes that are likely to cause the complete loss of the lands for agricultural activity.
On the contrary, the beans fields and pasture in the key-site are characterized by medium organic matter content of 1,61% è 1,68%. It should be mentioned that such low percentage is typical for the mountain soils of the territory. The organic matter index of more than 2% is considered to be a high one in accordance with the standards acceptable to the environmental conditions.
Table illustrates the analysis results presenting other meaningful indications of the soils in the key sectors.
Table.
THE SOIL PARAMETERS OF THE KEY-SITE SLOPES WITH INCLINATION ANGLE OF 10
|
Cultivation |
pH |
Nitrogen, % |
Phosphorus, ppm |
Potassium, cmol/kg |
Organic matter, % |
|
Pasture |
6.91 |
0.08 |
52.4 |
0.71 |
1.68 |
|
Cereals (Oats) |
7.16 |
0.04 |
96.6 |
0.21 |
0.88 |
|
Annual plants (Beans) |
7.18 |
0.08 |
64.8 |
0.76 |
1.61 |
|
Corn |
6.80 |
0.03 |
11.2 |
0.36 |
0.53 |
The analysis reveals that nitrogen content is low in the soils of all the sectors. According to the standards acceptable to Ecuador, the soils of the mountain zone are characterized by high phosphorus content in case they are used for the cultivation of cereals or beans and pastures. The medium phosphorus content is general for corn fields. The high index of potassium was defined in the soils of the sectors used for beans cultivation and permanent grass growing. The corn and cereals fields are characterized by the medium potassium index.
Prolong corn cultivation on the slopes with inclination angle of 10° leads to the considerable degradation of the soils in the mountain areas of Ecuador. The actions should be taken to change the policy of agricultural land use in the region; to turn to crop rotation is one of such measures.
It is recommended to reduce corn cultivation in steeply inclined areas unless erosion control measures are taken.
References: / Ñïèñîê ëèòåðàòóðû:
- 1. Kravchenko, R., & Guerrero, D. D. (2017). Comparative analysis of the eroded soils on the slopes of the Calderon region, Ecuador. Bulletin of Science and Practice, (3), 148-152. doi:10.5281/zenodo.399186.
- 2. De Noni, G., & Trujillo, G. (1990) Degradation del sudo en el Ecuador. Principales causas ó algunas reflexiones sobre la conservation de este recurso. Informe ORSTOM. Quito, Ecuador, 383-394. (In Spanish).
- 3. Mena, P. A., Josse C., & Medina, G. (2000). Los Suelos del Paramo. Serie Paramo 5. GTP/Abya Yala. Quito, 76. (In Spanish).
- 4. Flores, M. J. (2017). Evaluation ó consideration de los procesos de erosion en el uso racional de las tierras agricolas en la Provincia de Cotopaxi, Canton Latacunga, Parroquia Alaquez Trabajo previo a la obtencion del titulo de Ingeniero Ambiental ó Manejo de Riesgos Naturales. Quito, Universidad Tecnologica Equinoccial, 133. (In Spanish).
Ðàáîòà ïîñòóïèëà â ðåäàêöèþ 20.03.2017 ã.
Ïðèíÿòà ê ïóáëèêàöèè 22.03.2017ã.
Cite as (ÀÐÀ):
Kravchenko, R., & Flores, M. J. (2017). The characterization of the agricultural lands on the erosion-threatened slopes near Alaquez, Ecuador. Bulletin of Science and Practice, (4), 184-187.
Ññûëêà äëÿ öèòèðîâàíèÿ:
Êðàâ÷åíêî Ð. À., Ôëîðåñ Ì. X. Îöåíêà ñîñòîÿíèÿ ñåëüñêîõîçÿéñòâåííûõ çåìåëü íà ýðîçèîííî îïàñíûõ ñêëîíàõ â ðàéîíå Àëàêåñà, Ýêâàäîð // Áþëëåòåíü íàóêè è ïðàêòèêè. Ýëåêòðîí, æóðí. 2017. ¹4 (17). Ñ. 184 187. Ðåæèì äîñòóïà: http://www.bulletennauki.com/kravchenko-flores (äàòà îáðàùåíèÿ 15.04.2017). (Íà àíãë.).
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