Suitability Grouping System of Paddy Soils for Multiple Cropping -Part II : Criteria of the Suitability Grouping

다모작(多毛作)을 위한 답토양(畓土壤) 적성등급(適性等級) 구분(區分) -제(第)2보(報) : 적성등급(適性等級) 구분기준(區分基準)

To establish a suitability grouping system of paddy soils for multiple cropping of rice with other upland crops, the study was carried out after a few basic experiments. In succession to the results on basic experiment prior, the suitability system proposed and the results of application mentioned in this report were summarized as follows; 1. The factors of soil properties in the system were productivities represented by soil texture and drainage class, as well as salinity of surface and sub-soil pH of chemical properties were considered together with slope, warmth index, ground water table, parent materials etc. of soil physical or environmental conditions. The weights of the factors were combined with multiplicatively and additively so as the total marks of ideal soil to be 100. The system was composed with 5 suitability classes; over 91 mark is class I, under 60 mark class V, and each 10 point interval between classes. The limiting factors "P" (in the case that Physical properties or Productivity marks under 24), "S" (Surface slope less than 15) and "C" (Chemical condition below 15) etc. were appended up to two kinds to the classes except a part of soils in class I. 2. The areas where the warmth index exceed 110 in Yeongnam were 19% for class I, 22.7% for class II, 44.7% for class III, 11.5% for class IV, and 2.1% for class V. The rates in class I and II were slightly more than those of the whole country. 3. The points of each soil gained by the system had a positive correlation ($r=.922^{**}$) with the potential productivities.

논토양(土壤)에 수도(水稻)를 포함(包含)하여 그 전후작(前後作)으로 밭작물(作物)을 다모작(多毛作) 할 경우에 토양종류별(土壤種類別) 적성정도(適性程度)를 추정(推定) 할 수 있는 논토양다모작적성등급(土壤多毛作適性等級)을 구분(區分)코자 기초시험(基礎試驗)을 실시(實施)하고 적성등급구분(適性等級區分) 기준(基準)을 설정(設定)하였다. 기초시험결과(基礎試驗結果)는 전보(前報)에서 논(論)하였고 구분기준(區分基準) 및 주요결과(主要結果)는 다음과 같다. 1. 적성등급(適性等級) 구분요인(區分要因)은 잠재생산력을 대표(代表)한 토성(土性) 및 배수등급(排水等級), 화학적특성(化學的特性)(표토염농도(表土鹽濃度), 및 심토(心土)의 반응(反應)), 환경조건(環境條件)(경사도(傾斜度) 및 온량지수(溫量指數)) 그리고 지하수위(地下水位) 및 토양모재(土壤母材) 등(等)을 선택(選擇)하여 연역(演繹) 귀납(歸納) 절충식(折衷式) 인자별가중치(因子別加重値) 상승(相乘) 상가복합법(相加複合法)에 의한 이론적(理論的) 최상치(最上値)가 100 점(點)이 되도록 하였다. 91 점이상(點以上)인 토양(土壤)을 I급지(級地)로 하고 60 점이하(點以下)인 토양(土壤)을 V급지(級地)로 하되 10 점(點) 단위(單位)로 등분(等分)하였으며 등급별(等級別) 제한인자(制限因子)는 "물리성(物理性)" "화학성(化學性)" 및 "경사도(傾斜度)" 등(等) 3가지로 하되 2개까지 병기 가능(可能)토록 하였다. 2. 온량지수(溫量指數) 110 이상(以上)인 대부분(大部分)의 영남지역(嶺南地域)은 I급지(級地)가 19%, II급지(級地) 22.7%, III급지(級地) 44.7%, IV급지(級地) 11.5% 그리고 V급지(級地)가 2.1%로서 전국(全國)의 논토양(土壤) 급지별(級地別) 분포비율(分布比率)보다는 상급지비율(上級地比率)이 약간 높았다. 3. 토양별(土壤別) 총득점(總得點)과 생산력지수간에는 유의성(有意性)($r=.922^{**}$)이 인정(認定)되어 기준(基準)의 적합도(適合度)가 높은 것으로 볼 수 있었다.