• 한국초지조사료학회지
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• 제10권2호
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• pp.84-88
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• 1990

This experiment was conducted to evaluate the effect of cutting frequency and nitrogen fertilization on $(NO_3$-N leaching losses under 12 years mixture permanent meadow, The results of this study were summarized as follows: 1. There was no difference in the $(NO_3$-N content of soil water within 1 m soil depth during the whole experimental period. It means that the content of $(NO_3$-N leaching losses was not influenced by botanical composition, cutting frequency and nitrogen fertilization in this experiment. 2. The level of $(NO_3$-N content during the whole experimental period was not in excess of 0.5 ppm level.

• 한국초지조사료학회지
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• 제28권2호
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• pp.81-88
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• 2008

돈분액비의 DM 농도와 분시 차이가 동계사료작물의 생산성 및 토양특성에 미치는 영향을 비교하기 위해 2005년 11월부터 2006년 6월까지 제주특별자치도 축산진흥원 사료작물 포장에서 동계사료작물 호밀을 이용하여 수행되었다. 시험은 주구 2처리(고농도 DM 7.0%, 저농도 DM 1.6% 돈분액비), 세구 2처리(기비 100%, 기비 50%와 추비 50% 시용)를 각 각 4반복 분할구법으로 설계하였다. 고농도 돈분액비 시용이 저농도 액비 보다 호밀의 초장과 건물수량에 통계적으로 유의적 증가를 보였다(P<0.05). 호밀의 조단백질 함량은 액비를 기비만 시용하는 것 보다 분시하므로 증가하였다(P<0.05). 돈분액비 시용으로 호밀의 대량무기물(P, K, Ca, Mg 및 Na)이나 미량무기물(Cu, Fe, Mn 및 Zn) 함량에 차이를 주지 않았고 동계사료작물 호밀을 재배했던 토양의 이, 화학적 특성에도 분뇨처리 효과가 없었다. 다만 호밀의 평균 P함량 0.16%는 화본과 작물 적정수준 $0.2{\sim}0.4%$보다 부족했고 호밀재배 토양의 pH(5.5), OM(13.3%), 유효인산(47.6mg/kg) 및 Ca(2.75) 함량은 농경지 토양 수준 보다 부족하였다. 결론적으로 DM 7.0%의 고농도 액비시용은 DM 1.6%의 저농도 액비 보다 호밀의 생산성 향상을 가져 왔으나 재배 토양의 이, 화학적 특성에 변화를 주지 않았다.

• 한국초지조사료학회지
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• 제27권1호
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• pp.45-52
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• 2007

본 연구는 2003년 8월부터 2005년 12월까지 농촌진흥청 난지농업연구소의 기존 혼파 방목초지(해발 200m)에서 실시하였으며 방목 혼파초지에 우분퇴비 시용에 따른 사초생산성 및 토양 개선 효과를 구명하기 위하여 수행되었다. 화학비료 단용구, 우분퇴비 단용구, 화학 및 우분퇴비의 시용수준, 화학비료와 퇴비의 연차별 교호시용 등의 처리를 두어 우분퇴비 시용이 혼파초지의 사초생산성 및 토양성분에 미치는 영향을 조사하였다. 연간 총건물수량을 비교해보면 시험1년차에는 T1처리구가 11,342 kg/ha, 시험2년차에는 T5처리구가 13,468kg/ha, 3년차는 T6처리구가 10,724kg/ha로 가장 높은 수량을 보였으며 시험기간 동안 평균 건물수량은 화학비료구가 11,486kg/ha으로 가장 높은 건물생산성을 보였지만 처리 간 유의성은 없었다. 처리별 토양성분 변화는 퇴비구에서 화학비료구 보다 유효인산, 유기물 함량 등이 증가를 보임으로서 토양개선효과가 나타났으며 목초의 식생구성율은 처리구에 따라 큰 차이를 보이지 않았으며 봄철에는 화본과가 다소 높다가 여름철이 지나면서 두과와 잡초의 비율이 상승하는 경향을 보였다.

• Spatial Information Research
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• 제10권2호
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• pp.301-316
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• 2002

강우나 물의 유출에 의한 토양침식은 농업 생산성을 떨어뜨리고 목초지를 손상시키며, 물의 흐름을 방해하는 등의 각종 환경적인 문제를 야기시키고 있다. 또한 침식된 토사의 하천유입으로 저수지나 댐의 유효저수량이 감소되는 문제가 발생하고 있다. GIS를 연계하여 유역의 토양침식량을 추정하기 위해 수정범용토양손실공식(RUSLE)을 주로 활용하고 있으나, 실측자료와의 비교가 어려워 계산된 토양침식량을 정량적으로 평가하는 것은 큰 의미가 없다 본 연구에서는 RUSLE 모형으로 계산한 토양침식량의 정량적인 추정을 위해 보성강 유역의 비퇴사량 실측자료를 이용하였다. RUSLE 모형으로 계산한 비유사량과 비퇴사량 실측자료로부터 계산한 비유사량과의 비교 검토를 통해 RUSLE 계산에 적합한 해상도를 결정한 결과, 150m의 셀크기가 가장 적절한 것으로 평가되었다.

• Asian-Australasian Journal of Animal Sciences
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• 제6권1호
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• pp.107-113
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• 1993

This study determined the concentrations of micro-minerals in pastures, in feed supplements and in grazing, reproducing ewes, at different times during the year, at three farms in Northern China. Samples were collected 5 to 8 times during the year and analysed for selenium, copper, iron, molybdenum and zinc. On two farms selenium concentrations in both pastures and animal tissues were low for part of the year. The lowest concentrations in pasture (< $30{\mu}g/kg$ DM) and liver (< $100{\mu}g/kg$ wet weight) indicated that productivity of the sheep may be reduced by a deficiency of this element. On one farm copper concentrations in the lever were in the liver were in the deficient range (< $5{\mu}g/kg$ wet weight) for part of the year. It is likely that this is a result of high intakes of iron from pasture (up to 4.5 g Fe/kg DM) and soil, as indicated by high concentrations of iron in faeces (up to 7 g Fe/kg DM). Molybdenum intake is unlikely to have had much influence on copper absorption because pasture concentrations of this element were not unusually high (1 to 5 mg/kg DM). Zinc in pastures on two farms was below 10 mg/kg DM for part of the year. On one of these farms, the concentration of zinc in faeces was below 30 mg/kg DM throughout the year and this is consistent with zinc intakes of 7 to 15 mg/kg. Despite these low intakes, the concentratons of zinc in plasma were consistently above deficient levels. No clinical signs of deficiencies of any of the elements studied were observed.

• Asian-Australasian Journal of Animal Sciences
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• 제18권2호
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• pp.296-300
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• 2005

Human-induced soil salinity is becoming a major threat to agriculture across the world. This salinisation occurs in both irrigated and rain-fed agricultural zones with the highest proportions in the arid and semi-arid environments. Livestock can play an important role in the management and rehabilitation of this land. There are a range of plants that grow in saline soils and these have been used as animal feed. In many situations, animal production has been poor as a result of low edible biomass production, low nutritive value, depressed appetite, or a reduction in efficiency of energy use. Feeding systems are proposed that maximise the feeding value of plants growing on saline land and integrate their use with other feed resources available within mixed livestock and crop farming systems. Salt-tolerant pastures, particularly the chenopod shrubs, have moderate digestible energy and high crude protein. For this reason they represent a good supplement for poor quality pastures and crop residues. The use of salt-tolerant pasture systems not only provides feed for livestock but also may act as a bio-drain to lower saline water tables and improve the soil for growth of alternative less salt tolerant plants. In the longer term there are opportunities to identify and select more appropriate plants and animals for saline agriculture.

• 한국물환경학회지
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• 제25권6호
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• pp.910-915
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• 2009

The ecohydrologic characteristics according to planting in riparian zone for the riparian restoration are analyzed in this research. The ecohydrologic components due to land use change in riparian zone from existing land cover to planted area such as pasture and wildrye are simulated in the test basin with the integrated SWAT-MODFLOW model. After analysis of change of the hydrologic properties such as surface flow, lateral flow, transpiration and soil water in riparian zone, it is revealed that soil water is one of the key factors and planting of wildrye can increase soil water in riparian zone. The simulation performance of the SWAT-MODFLOW model is validated in this study and it is expected that this model can be used to evaluate various riparian restoration scenarios.

• 한국농공학회지
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• 제16권4호
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• pp.3555-3571
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• 1974

This experiment of which aim contribute to plan irrigation system so as to increase forage crop yields, was conducted to estimate evapotranspiration amount of forage crops and to find out system of consumed water in a pasture-ground. The results obtained by this study are as follows: 1. The general weather conditions which, were closely related to the evapotrannpiration of forage crops were nearly same as those of the average year with the exception that temperature of May and June were slightly low. 2. According to the investigation of potential evapotranspirations (P.E) or forage crops and its changes during growing periods, changes of tenday P.E. were high significant according to the harvesting period. P.E of Alfalfa of which yield was the largest was the biggest. Althrough the correlations between P.E. and meteorological factors were irregular oming to three-time harvesting, correlation between ten-day evapotraspiration amount and copper plated pan evaporation or solar radiation was high positive significant. 4. Predicting formulas of P.E. were led by weather factors, and also relatione between P.E. and weather factors were showed as figure. from the these formulas, P.E. may be calculated by weather factors. 5. Predicting formulas of P.E. were led by mean temperature and copper plated pan evaporation, and by mean temperature and solar radiation. As computed values and measured values showed in figure, these formulas were high signiflent. 6. In the total consumed soil water duration of 10 days which, was non-rain period from 12th to 21th of August, Alfalfa was the largest 48.1mm, second, Orchard grass 40.1mm and Fescue 37.6mm, and Ladino clover was the smallest 37.1mm, also, order of each forage crop yield amound. was same to the abov. Order of soil moisture extraction rate of soil layer of all the for forage crops dulation of ten-day was soil layer 1 which was largest, soil layer 2, 3, and 4 Reviewing the the first five-day and the second five day, in the first five-day, order of that of all the forage crops was same to the above, but in the second five-day, that of soil layer 2 or 3 was more than the of soil layer 1.

• 한국초지조사료학회지
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• 제17권1호
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• pp.43-50
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• 1997

The aim of the study is to describe the fate and transformation of nitrogen in grassland ecosystems. Field experiments were conducted using sandyloam soil under variabling conditions: Zen, fertilization, reduced slurry application(l20kg N $ha^{-1}\;yr^{-1}$), usual sluny application (240 kg N $ha^{-1}\;yr^{-1}$).Soil water samples were gathered with 120cm ceramic cups with initial pressure of 0.5 bar. Samples were collected twice a month and analysed for NO, colormetrically. Percolation was calculated as the difference between precipitation and potential evapotranspiration, and leaching as the product of percolation and nitrate content of the water h m the ceramic cups. The N$H_4$-N content in soil had no significant effect on slurry application, but high slurry application on grassland resulted in high N$O_3$-N content in soil. The NO, concentration in soil water was remarkably variable during the year. The average N$O_3$, concentration during experiment became the lowest(8.5 mg/e ) without slurry application and highest with 240kOa cattle sluny(25.3 mg4 ). For each of the three different amounts of cattle sluny applied (0, 120, and 240kOa), the amount of N$O_3$-N leached per year were 12, 23 and 29kg/ha respectively. On grassland under the climatic conditions of Allgau showed enormous nitrate leaching, which has a p a t potential of polluting the ground water. The high pool of mineral N in the soil are the source for N$O_3$ leaching. The leaching of N$O_3$ cannot be avoided completely, but minimized by optimizing N fertilization rate.

• 한국측량학회지
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• 제19권1호
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• pp.27-37
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• 2001

강우나 물의 유출에 의한 토양침식은 농업 생산성을 떨어뜨리고 목초지를 손상시키며, 물의 흐름을 방해하는 등의 각종 환경적인 문제를 야기시키고 있다. 환경에 대한 관심이 고조되는 시점에서 토양침식이 매우 중요한 위치를 차지하고 있지만 아직은 체계적인 자료의 정리와 분석이 이루어지지 못하고 있는 실정이다. 본 연구는 최근 부각되고 있는 GSIS를 활용하여 토양침식을 예측하는 모형에 입력되는 인자를 추출하는 기법을 제시하는 것으로 침식모형에는 ANSWER, WEPP RUSLE 등 여러 가지가 있으나 본 연구에서는 GSIS 자료와의 연계가 용이하면서 유역에 대한 일반적인 토양침식을 예측할 수 있는 RUSLE 침식모형을 사용하였다. RUSLE 입력인자에는 강우침식인자 R, 토양침식인자 K, 침식사면의 길이인자 L, 침식사면의 경사인자 S, 식생피복인자 C 그리고 경작인자 P로 구성되어 있다. RUSLE 입력인자 중 L과 S인자 추출에 사용되었던 기존의 식은 대부분 농업지역에 적용된 식으로 유역에 적용시 한계가 있기 때문에 본 연구에서는 GSIS 자료를 통해 격자별로 유역에 적용 가능한 수정된 경험식을 활용하였다. 또한 격자형 RUSLE인자를 유역추출 알고리즘을 이용하여 유역별로 분석함으로서 유역별 RUSLE인자의 최소값, 최대값, 평균 그리고 표준편차를 계산할 수 있었다.